Geomagnetic excursions are recognized as intrinsic features of the Earth's magnetic field. High-resolution records of field behaviour, captured in marine sedimentary cores, present an opportunity to determine the temporal and geometric character of the field during geomagnetic excursions and provide constraints on the mechanisms producing field variability. We present here the highest resolution record yet published of the Blake geomagnetic excursion (~125 ka) measured in three cores from Ocean Drilling Program (ODP) Site 1062 on the Blake-Bahama Outer Ridge. The Blake excursion has a controversial structure and timing but these cores have a sufficiently high sedimentation rate (~10cm/ka) to allow detailed reconstruction of the field behaviour at this site during the excursion. Palaeomagnetic measurements of the cores reveal rapid transitions (<500 yr) between the contemporary stable normal polarity and a completely reversed state of long duration which spans a stratigraphic interval of 0.7 m. We determine the duration of the reversed state during the Blake excursion using oxygen isotope stratigraphy, combined with 230Th excess measurements to assess variations in the sedimentation rates through the sections of interest. This provides an age and duration for the Blake excursion with greater accuracy and with constrained uncertainty. We date the directional excursion as falling between 129 and 122 ka with a duration for the deviation of 6.5±1.3 kyr. The long duration of this interval and the fully reversed field suggest the existence of a pseudo-stable, reversed dipole field component during the excursion and challenge the idea that excursions are always of short duration.

Standard Deviations of LCS products at 500km rolling 8-day resolution. Averaging performed by NetCDF Operators cdm_data_type=Grid Conventions=COARDS, CF-1.6, ACDD-1.3 Easternmost_Easting=177.5 geospatial_lat_max=87.46111111111111 geospatial_lat_min=-87.4611111111111 geospatial_lat_resolution=4.997777777777777 geospatial_lat_units=degrees_north geospatial_lon_max=177.5 geospatial_lon_min=-177.5 geospatial_lon_resolution=5.0 geospatial_lon_units=degrees_east history=Thu Mar 30 14:08:43 2023: ncrcat 0/1_day_2009_001.nc 0/1_day_2009_002.nc 0/1_day_2009_003.nc 0/1_day_2009_004.nc 0/1_day_2009_005.nc 0/1_day_2009_006.nc 0/1_day_2009_007.nc 0/1_day_2009_008.nc 0/1_day_2009_009.nc 0/1_day_2009_010.nc 0/1_day_2009_011.nc 0/1_day_2009_012.nc 0/1_day_2009_013.nc 0/1_day_2009_014.nc 0/1_day_2009_015.nc 0/1_day_2009_016.nc 0/1_day_2009_017.nc 0/1_day_2009_018.nc 0/1_day_2009_019.nc 0/1_day_2009_020.nc 0/1_day_2009_021.nc 0/1_day_2009_022.nc 0/1_day_2009_023.nc 0/1_day_2009_024.nc 0/1_day_2009_025.nc 0/1_day_2009_026.nc 0/1_day_2009_027.nc 0/1_day_2009_028.nc 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sourceUrl=(local files) Southernmost_Northing=-87.4611111111111 standard_name_vocabulary=CF Standard Name Table v70 time_coverage_end=2009-12-31T05:00:00Z time_coverage_start=2000-01-01T05:00:00Z Westernmost_Easting=-177.5

Hole 1105A penetrated 158 m of gabbros at a site offset 1.3 km east-northeast from Hole 735B on the Atlantis Bank near the Atlantis II Fracture Zone. A total of 118 m of dominantly medium- to coarse-grained intercalated Fe-Ti oxide gabbro and olivine gabbro was recovered from Hole 1105A that shows many petrographic features similar to those recovered from the upper part of Hole 735B. The main rock types are distinguished based on the constituent cumulus phases, with the most primitive gabbros consisting of olivine, plagioclase, and clinopyroxene. The inferred crystallization order is subsequently Fe-Ti oxides (ilmenite and titanomagnetite), followed by orthopyroxene, then apatite, and finally biotite. Orthopyroxene appears to replace olivine in a narrow middle interval. The magmatic evolution is likewise reflected in the mineral compositions. Plagioclase varies from An66 to An28. Olivine varies from Fo78 to Fo35. The gap in olivine crystallization occurs between Fo46 and Fo40 and coincides approximately with the appearance of orthopyroxene (~En50). The clinopyroxenes show large compositional variation in Mg/(Mg + Fe total) from 0.84 to 0.51. The nonquadrilateral cations of clinopyroxene similarly show large variations with Ti increasing for the olivine gabbros and decreasing for the Fe-Ti oxide gabbros with the decrease in Mg/(Mg + Fe total). The apatites are mainly flourapatites. The compositional variation in the gabbros is interpreted as a comagmatic suite resulting from fractional crystallization. Pyroxene geothermometry suggests equilibration temperatures from 1100°C and below. The coexisting Fe-Ti oxide minerals indicate subsolidus equilibration temperatures from 900°C for olivine gabbros to 700°C for the most evolved apatite-bearing gabbros. The cryptic variation in the olivine gabbros defines two or three lenses, 40 to 60 m thick, each characterized by a distinct convex zoning with a lower segment indicating upward reverse fractionation, a central maximum, and an upper segment showing normal fractionation. The Fe-Ti oxide gabbros show cryptic variations independent of the host olivine gabbros and reveal a systematic upward normal fractionation trend transgressing host olivine gabbro boundaries. Forward fractional crystallization modeling, using a likely parental magma composition from the Atlantis II Fracture Zone (MgO = 7.2 wt%; Mg/[Mg + Fe2+] = 0.62), closely matches the compositions of coexisting olivine, plagioclase, and clinopyroxene. This modeling suggests cosaturation of olivine, plagioclase, and clinopyroxene from 1155°C and the addition of Fe-Ti oxides from 1100°C. The liquid line of descent initially shows increasing FeO with moderately increasing SiO2. After saturation of Fe-Ti oxides, the liquid strongly decreases in FeO and TiO2 and increases in SiO2, reaching dacitic compositions at ~10% liquid remaining. The calculations indicate that formation of olivine gabbros can be accounted for by <65% fractionation and that only the residual 35% liquid was saturated in Fe-Ti oxides. The modeling of the solid fractionation products shows that both the olivine gabbro and the Fe-Ti oxide gabbros contain very small amounts of trapped liquid (<5%). The implications are that the gabbros represent crystal mush that originated in a recharging and tapping subaxial chamber. Compaction and upward melt migration in the crystal mush appear to have been terminated with relatively large amounts of interstitial liquid remaining in the upper parts of the cumulate mush. This termination may have been caused by tectonic disturbances, uplift, and associated withdrawal of magma into the subaxial dike and sill system. Prolonged compaction and cooling of the trapped melt in the mush formed small differentiated bodies and lenses by pressure release migration and crystallization along syntectonic channels. This resulted in differentiation products along lateral and vertical channelways in the host gabbro that vary from olivine gabbro, to Fe-Ti oxide gabbro, gabbronorite, and apatite gabbros and show large compositional variations independent of the host olivine gabbros.

Eolian dust is a significant source of iron and other nutrients that are essential for the health of marine ecosystems and potentially a controlling factor of the high nutrient-low chlorophyll status of the Subarctic North Pacific. We map the spatial distribution of dust input using three different geochemical tracers of eolian dust, 4He, 232Th and rare earth elements, in combination with grain size distribution data, from a set of core-top sediments covering the entire Subarctic North Pacific. Using the suite of geochemical proxies to fingerprint different lithogenic components, we deconvolve eolian dust input from other lithogenic inputs such as volcanic ash, ice-rafted debris, riverine and hemipelagic input. While the open ocean sites far away from the volcanic arcs are dominantly composed of pure eolian dust, lithogenic components other than eolian dust play a more crucial role along the arcs. In sites dominated by dust, eolian dust input appears to be characterized by a nearly uniform grain size mode at ~4 µm. Applying the 230Th-normalization technique, our proxies yield a consistent pattern of uniform dust fluxes of 1-2 g/m**2/yr across the Subarctic North Pacific. Elevated eolian dust fluxes of 2-4 g/m**2/yr characterize the westernmost region off Japan and the southern Kurile Islands south of 45° N and west of 165° E along the main pathway of the westerly winds. The core-top based dust flux reconstruction is consistent with recent estimates based on dissolved thorium isotope concentrations in seawater from the Subarctic North Pacific. The dust flux pattern compares well with state-of-the-art dust model predictions in the western and central Subarctic North Pacific, but we find that dust fluxes are higher than modeled fluxes by 0.5-1 g/m**2/yr in the northwest, northeast and eastern Subarctic North Pacific. Our results provide an important benchmark for biogeochemical models and a robust approach for downcore studies testing dust-induced iron fertilization of past changes in biological productivity in the Subarctic North Pacific.

The results of a search for a standard model-like Higgs boson decaying into two photons in the mass range between 70 and 110 GeV are presented. The analysis uses the data set collected by the CMS experiment in proton-proton collisions at $\sqrt{s}$ = 13 TeV corresponding to integrated luminosities of 36.3 fb$^{-1}$, 41.5 fb$^{-1}$ and 54.4 fb$^{-1}$ during the 2016, 2017, and 2018 LHC running periods, respectively. No significant excess over the background expectation is observed and 95% confidence level upper limits are set on the product of the cross section and branching fraction for decays of an additional Higgs boson into two photons. The maximum deviation with respect to the background is seen for a mass hypothesis of 95.4 GeV with a local (global) significance of 2.9 (1.3) standard deviations. The observed upper limit ranges from 15 to 73 fb.

ONC, Strait of Georgia, BC Ferries, Tsawwassen - Duke Point, 1min, v18-01

Data from the Ocean Networks Canada (ONC) Strait of Georgia Mobile Platforms, British Columbia Ferries, Tsawwassen - Duke Point route. The data are resampled from the raw instrument data to 1 minute mean values. They are accompanied by standard deviations and sample counts for each of the 1 minute aggregation intervals.

v1: on_crossing_mask, crossing_number, temperature, temperature standard deviation, temperature sample counts, conductivity, conductivity standard deviation, conductivity sample counts, reference salinity, reference salinity standard deviation, reference salinity sample counts, O2 saturation, O2 saturation standard deviation, O2 saturation sample counts, corrected O2 concentration, corrected O2 concentration standard deviation, corrected O2 concentration sample counts, O2 sensor temperature, O2 sensor temperature standard deviation, O2 sensor temperature sample counts, CDOM fluorescence, CDOM fluorescence standard deviation, CDOM fluorescence sample counts, chlorophyll, chlorophyll standard deviation, chlorophyll sample counts, turbidity, turbidity standard deviation, turbidity sample counts, CO2 partial pressure, CO2 partial pressure standard deviation, CO2 partial pressure sample counts, linearized CO2 concentration, linearized CO2 concentration standard deviation, linearized CO2 concentration sample counts, variables v18-01: Add air temperature, air temperature standard deviation, air temperature sample counts, relative humidity, relative humidity standard deviation, relative humidity sample counts, barometric pressure, barometric pressure standard deviation, barometric pressure sample counts, solar radiation, solar radiation standard deviation, solar radiation sample counts, longwave radiation, longwave radiation standard deviation, longwave radiation sample counts, variables acknowledgement=Ocean Networks Canada (ONC) cdm_data_type=TimeSeries cdm_timeseries_variables=longitude, latitude, on_crossing_mask, crossing_number Conventions=CF-1.6, COARDS, ACDD-1.3 drawLandMask=over Easternmost_Easting=-122.98946356897223 featureType=TimeSeries ferry_route_name=Tsawwassen - Duke Point geospatial_lat_max=49.443338394749986 geospatial_lat_min=48.38421507991666 geospatial_lat_units=degrees_north geospatial_lon_max=-122.98946356897223 geospatial_lon_min=-123.958475 geospatial_lon_units=degrees_east history=Download raw data from ONC scalardata API. Filter to exclude data with qaqcFlag != 1. Resample data to 1 minute intervals using mean, standard deviation and count as aggregation functions. Store as netCDF4 file. infoUrl=https://salishsea.eos.ubc.ca/ institution=UBC EOAS institution_fullname=Dept of Earth, Ocean & Atmospheric Sciences, University of British Columbia keywords_vocabulary=GCMD Science Keywords Northernmost_Northing=49.443338394749986 ONC_stationDescription=Mobile Platforms, British Columbia Ferries, Tsawwassen - Duke Point project=SalishSeaCast NEMO Model sourceUrl=(local files) Southernmost_Northing=48.38421507991666 standard_name_vocabulary=CF Standard Name Table v29 testOutOfDate=now-2days time_coverage_end=2024-12-20T23:58:00Z time_coverage_start=2012-05-10T00:00:00Z Westernmost_Easting=-123.958475

Walton-Smith Conductivity, Temperature, Depth (CTD) - WS23010 - WS23010_WS23011_Kelble_Stn.031 - 2023-01-15 - 25.74N 81.9412W. Hydrographic Measurements in the Gulf of Mexico. flags: 1 = good; 3 = mean ± 3*standard deviation; 4 = mean ± 5*standard deviation; 9 = missing. other acknowledgement=other cdm_altitude_proxy=depth cdm_data_type=Profile cdm_profile_variables=profile, time, latitude, longitude, platform, instrument, instrument1, instrument2, instrument3, instrument4, instrument5, instrument6, instrument7, instrument8, instrument9, instrument10, instrument11, instrument12, instrument13, crs comment=Processing:datcnv_ox_hysteresis_correction = yes; datcnv_ox_tau_correction = yes; filter_low_pass_tc_A = 0.030; filter_low_pass_tc_B = 0.150; filter_low_pass_A_vars = CStarAt0 CStarTr0, par, dz/dtM; filter_low_pass_B_vars = prDM ;alignctd_adv = c0S/m 0.073, c1S/m 0.073, sbeox0ML/L 3.500, oxsatML/L 3.500; celltm_alpha = 0.0300, 0.0300; celltm_tau = 7.0000, 7.0000; loopedit_minVelocity = 0.010; loopedit_surfaceSoak = 1: minDepth = 0.5, maxDepth = 2; useDeckPress = 1; loopedit_excl_bad_scans = yes comment1=flags: 1 = good; 3 = mean ± 3*standard deviation; 4 = mean ± 5*standard deviation; 9 = missing comment2=other contributor_country=USA contributor_email=other contributor_institution=other contributor_name=other contributor_phone=other contributor_role=other contributor_role_vocabulary=https://vocab.nerc.ac.uk/collection/G04/current/ contributor_url=other Conventions=CF-1.6, ACDD-1.3, IOOS-1.2, COARDS Country=USA date_metadata_modified=2023-06-27T11:15:41Z Easternmost_Easting=-81.94116666666666 featureType=Profile geospatial_bounds=POLYGON ((24.00 -83.00, 26.00, -83.00, 26.00, -80.00, 24.00 -80.00, 24.00 -83.00)) geospatial_bounds_crs=EPSG:4326 geospatial_bounds_vertical_crs=EPSG:5831 geospatial_lat_max=25.74 geospatial_lat_min=25.74 geospatial_lat_units=degrees_north geospatial_lon_max=-81.94116666666666 geospatial_lon_min=-81.94116666666666 geospatial_lon_units=degrees_east geospatial_vertical_max=14.943 geospatial_vertical_min=1.832 geospatial_vertical_positive=down geospatial_vertical_resolution=0.0033390637397513884 geospatial_vertical_units=m grid_mapping_FillValue=-999 grid_mapping_epsg_code=EPSG:4326 grid_mapping_inverse_flattening=298.257223563 grid_mapping_long_name=grid mapping variable for horizontal spatial coordinate reference system (CRS) grid_mapping_longitude_of_prime_meridian=0.0 grid_mapping_missing_value=-999.0 grid_mapping_name=latitude_longitude grid_mapping_semi_major_axis=6378137.0 grid_mapping_standard_name_url=http://mmisw.org/ont/cf/parameter/other grid_mapping_units=other history=2023-06-27T11:13:45Z id=WS23010 infoUrl=https://www.aoml.noaa.gov/phod/sfp/index.php institution=NOAA's Atlantic Oceanographic and Meteorological Laboratory/Ocean Chemistry and Ecosystems Division instrument=CTD Sea-Bird SBE-911plus instrument_vocabulary=GCMD Science Keywords Version 9.1.5 keywords_vocabulary=GCMD Science Keywords metadata_link=https://gcoos5.geos.tamu.edu/erddap/tabledap/Walton-Smith_WS23010_WS23010_WS23011_Kelble_Stn.031.html naming_authority=aoml.noaa.gov Northernmost_Northing=25.74 platform=RV_FG_Walton_Smith platform_id=other platform_name=RV_FG_Walton_Smith platform_vocabulary=https://mmisw.org/ont/ioos/platform processing_level=Geophysical units from raw data program=Florida Keys Monitoring program project=Marine Biodiversity Observation Network references=https://ocean.floridamarine.org/FKNMS_WQPP/ sea_name=Gulf of Mexico source=Rolling Deck to Repository (R2R) Program sourceUrl=(local files) Southernmost_Northing=25.74 standard_name_vocabulary=CF Standard Name Table v72 station_name=WS23010_WS23011_Kelble_Stn.031 subsetVariables=profile, time, latitude, longitude, platform, instrument, instrument1, instrument2, instrument3, instrument4, instrument5, instrument6, instrument7, instrument8, instrument9, instrument10, instrument11, instrument12, instrument13, crs time_coverage_duration=P00Y0M00DT00H00M00S time_coverage_end=2023-01-15T22:50:24Z time_coverage_resolution=other time_coverage_start=2023-01-15T22:50:24Z Westernmost_Easting=-81.94116666666666

Standard Deviations of AVHRR products at 100km rolling 8-day resolution. Averaging performed by NetCDF Operators cdm_data_type=Grid Conventions=COARDS, CF-1.6, ACDD-1.3 Easternmost_Easting=179.72222222222217 geospatial_lat_max=89.49724279835391 geospatial_lat_min=-89.12703703703703 geospatial_lat_resolution=0.925514403292181 geospatial_lat_units=degrees_north geospatial_lon_max=179.72222222222217 geospatial_lon_min=-179.53703703703704 geospatial_lon_resolution=0.9259259259259258 geospatial_lon_units=degrees_east history=Wed Oct 19 06:31:06 2022: ncrcat 0/1_day_2009_001.nc 0/1_day_2009_002.nc 0/1_day_2009_003.nc 0/1_day_2009_004.nc 0/1_day_2009_005.nc 0/1_day_2009_006.nc 0/1_day_2009_007.nc 0/1_day_2009_008.nc 0/1_day_2009_009.nc 0/1_day_2009_010.nc 0/1_day_2009_011.nc 0/1_day_2009_012.nc 0/1_day_2009_013.nc 0/1_day_2009_014.nc 0/1_day_2009_015.nc 0/1_day_2009_016.nc 0/1_day_2009_017.nc 0/1_day_2009_018.nc 0/1_day_2009_019.nc 0/1_day_2009_020.nc 0/1_day_2009_021.nc 0/1_day_2009_022.nc 0/1_day_2009_023.nc 0/1_day_2009_024.nc 0/1_day_2009_025.nc 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4.7.6 (Homepage = http://nco.sf.net, Code = https://github.com/nco/nco) Northernmost_Northing=89.49724279835391 sourceUrl=(local files) Southernmost_Northing=-89.12703703703703 standard_name_vocabulary=CF Standard Name Table v70 time_coverage_end=2009-12-31T05:00:00Z time_coverage_start=2000-01-01T05:00:00Z Westernmost_Easting=-179.53703703703704

Walton-Smith Conductivity, Temperature, Depth (CTD) - WS23010 - WS23010_WS23011_Kelble_Stn.033 - 2023-01-15 - 25.9097N 81.797W. Hydrographic Measurements in the Gulf of Mexico. flags: 1 = good; 3 = mean ± 3*standard deviation; 4 = mean ± 5*standard deviation; 9 = missing. other acknowledgement=other cdm_altitude_proxy=depth cdm_data_type=Profile cdm_profile_variables=profile, time, latitude, longitude, platform, instrument, instrument1, instrument2, instrument3, instrument4, instrument5, instrument6, instrument7, instrument8, instrument9, instrument10, instrument11, instrument12, instrument13, crs comment=Processing:datcnv_ox_hysteresis_correction = yes; datcnv_ox_tau_correction = yes; filter_low_pass_tc_A = 0.030; filter_low_pass_tc_B = 0.150; filter_low_pass_A_vars = CStarAt0 CStarTr0, par, dz/dtM; filter_low_pass_B_vars = prDM ;alignctd_adv = c0S/m 0.073, c1S/m 0.073, sbeox0ML/L 3.500, oxsatML/L 3.500; celltm_alpha = 0.0300, 0.0300; celltm_tau = 7.0000, 7.0000; loopedit_minVelocity = 0.010; loopedit_surfaceSoak = 1: minDepth = 0.5, maxDepth = 2; useDeckPress = 1; loopedit_excl_bad_scans = yes comment1=flags: 1 = good; 3 = mean ± 3*standard deviation; 4 = mean ± 5*standard deviation; 9 = missing comment2=other contributor_country=USA contributor_email=other contributor_institution=other contributor_name=other contributor_phone=other contributor_role=other contributor_role_vocabulary=https://vocab.nerc.ac.uk/collection/G04/current/ contributor_url=other Conventions=CF-1.6, ACDD-1.3, IOOS-1.2, COARDS Country=USA date_metadata_modified=2023-06-27T11:15:52Z Easternmost_Easting=-81.797 featureType=Profile geospatial_bounds=POLYGON ((24.00 -83.00, 26.00, -83.00, 26.00, -80.00, 24.00 -80.00, 24.00 -83.00)) geospatial_bounds_crs=EPSG:4326 geospatial_bounds_vertical_crs=EPSG:5831 geospatial_lat_max=25.909666666666666 geospatial_lat_min=25.909666666666666 geospatial_lat_units=degrees_north geospatial_lon_max=-81.797 geospatial_lon_min=-81.797 geospatial_lon_units=degrees_east geospatial_vertical_max=8.402 geospatial_vertical_min=2.074 geospatial_vertical_positive=down geospatial_vertical_resolution=0.0020082958866228825 geospatial_vertical_units=m grid_mapping_FillValue=-999 grid_mapping_epsg_code=EPSG:4326 grid_mapping_inverse_flattening=298.257223563 grid_mapping_long_name=grid mapping variable for horizontal spatial coordinate reference system (CRS) grid_mapping_longitude_of_prime_meridian=0.0 grid_mapping_missing_value=-999.0 grid_mapping_name=latitude_longitude grid_mapping_semi_major_axis=6378137.0 grid_mapping_standard_name_url=http://mmisw.org/ont/cf/parameter/other grid_mapping_units=other history=2023-06-27T11:13:45Z id=WS23010 infoUrl=https://www.aoml.noaa.gov/phod/sfp/index.php institution=NOAA's Atlantic Oceanographic and Meteorological Laboratory/Ocean Chemistry and Ecosystems Division instrument=CTD Sea-Bird SBE-911plus instrument_vocabulary=GCMD Science Keywords Version 9.1.5 keywords_vocabulary=GCMD Science Keywords metadata_link=https://gcoos5.geos.tamu.edu/erddap/tabledap/Walton-Smith_WS23010_WS23010_WS23011_Kelble_Stn.033.html naming_authority=aoml.noaa.gov Northernmost_Northing=25.909666666666666 platform=RV_FG_Walton_Smith platform_id=other platform_name=RV_FG_Walton_Smith platform_vocabulary=https://mmisw.org/ont/ioos/platform processing_level=Geophysical units from raw data program=Florida Keys Monitoring program project=Marine Biodiversity Observation Network references=https://ocean.floridamarine.org/FKNMS_WQPP/ sea_name=Gulf of Mexico source=Rolling Deck to Repository (R2R) Program sourceUrl=(local files) Southernmost_Northing=25.909666666666666 standard_name_vocabulary=CF Standard Name Table v72 station_name=WS23010_WS23011_Kelble_Stn.033 subsetVariables=profile, time, latitude, longitude, platform, instrument, instrument1, instrument2, instrument3, instrument4, instrument5, instrument6, instrument7, instrument8, instrument9, instrument10, instrument11, instrument12, instrument13, crs time_coverage_duration=P00Y0M00DT00H00M00S time_coverage_end=2023-01-15T21:11:43Z time_coverage_resolution=other time_coverage_start=2023-01-15T21:11:43Z Westernmost_Easting=-81.797

Sampling and Analytical Methodology: Samples were taken using 24 internally Teflon-coated PVC 12 litre GO-FLO Samplers (General Oceanics Inc.) mounted on an all-titanium frame (De Baar et al., 2008). This frame was connected to a 17.7 mm diameter Kevlar hydrowire with seven independent internal signal/conductor cables (Cousin Trestec S.A.) and controlled from onboard. Each GO-FLO sampler had a special ultraclean all-teflon PTFE valve (Cole Parmer; PN A-06392-31) installed. Samples for trace metal analysis were collected from the GO-FLO bottles in a class 100 clean room environment. The water was filtered over a 0.2 μm filter cartridge (Sartrobran-300, Sartorius) under pressure (1.5 atm) of (in-line prefiltered) nitrogen gas exerted via a special connector instead of the regular air bleeding valve at the top of each GO-FLO sampler. Sub-samples for Mn were taken in cleaned LDPE sample bottles (125 mL) from each GO-FLO bottle. All sample bottles were rinsed five times with the sample seawater. Analyses of dissolved Manganese (Mn) were performed on shipboard with the method developed by Doi et al. (2004) with some slight modifications in the preparation and brands of the chemicals used. Furthermore, samples were buffered in-line with an ammonium borate sample buffer (see text below). Samples were acidified with 12 M ultraclean HCl (Baseline® Hydrochloric Acid, Seastar Chemicals Inc.) to a pH of 1.8 and stored inside double plastic bags in plastic crates. At the home institute, in a flow injection system, the samples were buffered in-line to a pH of 8.5 ± 0.2 with ammonium borate sample buffer. This buffer was produced by dissolving 30.9 grams of boric acid (Suprapure, Merck) in 1 L MQ water and adjusting the pH to 9.4 with ammonium hydroxide (Suprapure, Merck). Dissolved Mn in the buffered sample was preconcentrated for 200 seconds on a Toyopearl AFChelate 650M (TesoHaas, Germany) column. Hereafter the column was rinsed for 60 seconds with MQ water to remove interfering salts. The Mn was subsequently eluted from the column for 200 seconds with a solution of 0.1M three times quartz distilled formic acid (reagent grade, Merck) containing 0.1 M hydrogen peroxide (Suprapure, Merck) and 12 mM ammonium hydroxide (Suprapure, Merck). The pH of this carrier solution was adjusted to 2.9 ± 0.05. The eluate with the dissolved Mn passed a second column of immobilized 8-hydroxyquinoline (Landing et al., 1986) to remove interfering iron ions in the carrier solution (Doi et al., 2004). Hereafter the carrier mixed subsequently with 0.7 M ammonium hydroxide (Suprapure Merck) and a luminol solution. The latter luminol solution was made by diluting 600 μl luminol stock solution and 10 μl TETA (triethylenetetramine, Merck) in 1 L MQ. The luminol stock solution was made by diluting 270 mg luminol (3-aminophtalhydrazide, Aldrich) and 500 mg potassium carbonate in 15 ml MQ. The resulting mixture of carrier solution, ammonium hydroxide and luminol solution had a pH of 10.2 ± 0.05 and entered a 3 meter length mixing coil placed in a water bath of 25°C. Hereafter the chemiluminescence was detected with a Hamamatsu HC135 Photon counter. Concentrations of dissolved Mn were calculated in nanomol•L-1 (nM) from the photon emission peak height (see below). The system was calibrated using standard additions from a 5000 nM Mn stock solution (Fluka) to filtered acidified seawater of low Mn concentration that was collected in Antarctic Ocean. A five-points calibration line (0, 0.15, 0.36, 0.73 and 1.46 nM standard additions) and blank determination were made daily. The three lowest points (0, 0.15 and 0.36 nM) of the calibration line were measured in triplicate and the two highest points (0.73 and 1.46 nM) in duplicate to add more weight to the lower part of the calibration line. The blank was determined by measuring column-cleaned seawater. Latter was obtained by passing seawater over a Toyopearl AFChelate 650M and an 8-hydroxyquinoline column which retained the dissolved Mn. The average blank value was 20 pM. The limit of detection defined as three times the standard deviation of the blank was < 0.01 nM. The flow injection system was rinsed every day with a 0.5 M HCl solution.

Data Processing: The system was calibrated using standard additions from a 5000 nM Mn stock solution (Fluka) to filtered acidified seawater of low Mn concentration that was collected in Antarctic Ocean. A five-points calibration line (0, 0.15, 0.36, 0.73 and 1.46 nM standard additions) and blank determination were made daily. The three lowest points (0, 0.15 and 0.36 nM) of the calibration line were measured in triplicate and the two highest points (0.73 and 1.46 nM) in duplicate to add more weight to the lower part of the calibration line. The blank was determined by measuring column-cleaned seawater. Latter was obtained by passing seawater over a Toyopearl AFChelate 650M and an 8-hydroxyquinoline column which retained the dissolved Mn. The average blank value was 20 pM. The limit of detection defined as three times the standard deviation of the blank was < 0.01 nM. The flow injection system was rinsed every day with a 0.5 M HCl solution. A standard was measured in triplicate every day. This standard was a sub-sample of a 25 L volume of filtered seawater that was taken at the beginning of the cruise. This standard was analysed 40 times on different days and the relative standard deviation of the replicate analysis in triplicate was 3.2%. The relative standard deviation on the separate days was on average 1.3 %. The average concentration of Mn of this standard was 0.44 nM and the deviation from this average for a given measuring day was used as a correction factor. To verify whether this correction was decreasing the inter-daily variability in the dataset, every day a sample which was collected and measured the previous measuring day, was analysed once again. The deviation between the concentrations measured on the different days decreased from 3.5% to 2.5%, indicating the data correction procedure is beneficial. As an independent comparison, the certification samples collected on the SAFe cruise (Johnson et al., 2007) were analysed for Mn. As an independent comparison, the certification samples collected on the American SAFe cruise (Johnson et al., 2007) were analysed in triplicate for Mn. The resulting concentrations of Mn for both SAFe Surface (S) and SAFe deep (D2) from 1000 m, agreed very nicely the community consensus value that is starting to emerge on the absolute concentrations of Mn in the SAFe samples. The dataset was scanned for obvious outliers and these have been quality flagged with the number 4. Some samples gave anomalous nutrient results for the intended depth and were assumed to have been closed at the wrong depth and quality flagged with the number 8. All other values are assumed to be correct and flagged with the number 0.

Standard Deviations of OSCAR products at 50km rolling 8-day resolution cdm_data_type=Grid Conventions=COARDS, CF-1.6, ACDD-1.3 Easternmost_Easting=179.75 geospatial_lat_max=89.70976356050069 geospatial_lat_min=-89.96 geospatial_lat_resolution=0.5004728789986091 geospatial_lat_units=degrees_north geospatial_lon_max=179.75 geospatial_lon_min=-179.75 geospatial_lon_resolution=0.5 geospatial_lon_units=degrees_east history=Thu Feb 1 07:26:13 2024: ncrcat 0/1_day_2009_001.nc 0/1_day_2009_002.nc 0/1_day_2009_003.nc 0/1_day_2009_004.nc 0/1_day_2009_005.nc 0/1_day_2009_006.nc 0/1_day_2009_007.nc 0/1_day_2009_008.nc 0/1_day_2009_009.nc 0/1_day_2009_010.nc 0/1_day_2009_011.nc 0/1_day_2009_012.nc 0/1_day_2009_013.nc 0/1_day_2009_014.nc 0/1_day_2009_015.nc 0/1_day_2009_016.nc 0/1_day_2009_017.nc 0/1_day_2009_018.nc 0/1_day_2009_019.nc 0/1_day_2009_020.nc 0/1_day_2009_021.nc 0/1_day_2009_022.nc 0/1_day_2009_023.nc 0/1_day_2009_024.nc 0/1_day_2009_025.nc 0/1_day_2009_026.nc 0/1_day_2009_027.nc 0/1_day_2009_028.nc 0/1_day_2009_029.nc 0/1_day_2009_030.nc 0/1_day_2009_031.nc 0/1_day_2009_032.nc 0/1_day_2009_033.nc 0/1_day_2009_034.nc 0/1_day_2009_035.nc 0/1_day_2009_036.nc 0/1_day_2009_037.nc 0/1_day_2009_038.nc 0/1_day_2009_039.nc 0/1_day_2009_040.nc 0/1_day_2009_041.nc 0/1_day_2009_042.nc 0/1_day_2009_043.nc 0/1_day_2009_044.nc 0/1_day_2009_045.nc 0/1_day_2009_046.nc 0/1_day_2009_047.nc 0/1_day_2009_048.nc 0/1_day_2009_049.nc 0/1_day_2009_050.nc 0/1_day_2009_051.nc 0/1_day_2009_052.nc 0/1_day_2009_053.nc 0/1_day_2009_054.nc 0/1_day_2009_055.nc 0/1_day_2009_056.nc 0/1_day_2009_057.nc 0/1_day_2009_058.nc 0/1_day_2009_059.nc 0/1_day_2009_060.nc 0/1_day_2009_061.nc 0/1_day_2009_062.nc 0/1_day_2009_063.nc 0/1_day_2009_064.nc 0/1_day_2009_065.nc 0/1_day_2009_066.nc 0/1_day_2009_067.nc 0/1_day_2009_068.nc 0/1_day_2009_069.nc 0/1_day_2009_070.nc 0/1_day_2009_071.nc 0/1_day_2009_072.nc 0/1_day_2009_073.nc 0/1_day_2009_074.nc 0/1_day_2009_075.nc 0/1_day_2009_076.nc 0/1_day_2009_077.nc 0/1_day_2009_078.nc 0/1_day_2009_079.nc 0/1_day_2009_080.nc 0/1_day_2009_081.nc 0/1_day_2009_082.nc 0/1_day_2009_083.nc 0/1_day_2009_084.nc 0/1_day_2009_085.nc 0/1_day_2009_086.nc 0/1_day_2009_087.nc 0/1_day_2009_088.nc 0/1_day_2009_089.nc 0/1_day_2009_090.nc 0/1_day_2009_091.nc 0/1_day_2009_092.nc 0/1_day_2009_093.nc 0/1_day_2009_094.nc 0/1_day_2009_095.nc 0/1_day_2009_096.nc 0/1_day_2009_097.nc 0/1_day_2009_098.nc 0/1_day_2009_099.nc 1/1_day_2009_100.nc 1/1_day_2009_101.nc 1/1_day_2009_102.nc 1/1_day_2009_103.nc 1/1_day_2009_104.nc 1/1_day_2009_105.nc 1/1_day_2009_106.nc 1/1_day_2009_107.nc 1/1_day_2009_108.nc 1/1_day_2009_109.nc 1/1_day_2009_110.nc 1/1_day_2009_111.nc 1/1_day_2009_112.nc 1/1_day_2009_113.nc 1/1_day_2009_114.nc 1/1_day_2009_115.nc 1/1_day_2009_116.nc 1/1_day_2009_117.nc 1/1_day_2009_118.nc 1/1_day_2009_119.nc 1/1_day_2009_120.nc 1/1_day_2009_121.nc 1/1_day_2009_122.nc 1/1_day_2009_123.nc 1/1_day_2009_124.nc 1/1_day_2009_125.nc 1/1_day_2009_126.nc 1/1_day_2009_127.nc 1/1_day_2009_128.nc 1/1_day_2009_129.nc 1/1_day_2009_130.nc 1/1_day_2009_131.nc 1/1_day_2009_132.nc 1/1_day_2009_133.nc 1/1_day_2009_134.nc 1/1_day_2009_135.nc 1/1_day_2009_136.nc 1/1_day_2009_137.nc 1/1_day_2009_138.nc 1/1_day_2009_139.nc 1/1_day_2009_140.nc 1/1_day_2009_141.nc 1/1_day_2009_142.nc 1/1_day_2009_143.nc 1/1_day_2009_144.nc 1/1_day_2009_145.nc 1/1_day_2009_146.nc 1/1_day_2009_147.nc 1/1_day_2009_148.nc 1/1_day_2009_149.nc 1/1_day_2009_150.nc 1/1_day_2009_151.nc 1/1_day_2009_152.nc 1/1_day_2009_153.nc 1/1_day_2009_154.nc 1/1_day_2009_155.nc 1/1_day_2009_156.nc 1/1_day_2009_157.nc 1/1_day_2009_158.nc 1/1_day_2009_159.nc 1/1_day_2009_160.nc 1/1_day_2009_161.nc 1/1_day_2009_162.nc 1/1_day_2009_163.nc 1/1_day_2009_164.nc 1/1_day_2009_165.nc 1/1_day_2009_166.nc 1/1_day_2009_167.nc 1/1_day_2009_168.nc 1/1_day_2009_169.nc 1/1_day_2009_170.nc 1/1_day_2009_171.nc 1/1_day_2009_172.nc 1/1_day_2009_173.nc 1/1_day_2009_174.nc 1/1_day_2009_175.nc 1/1_day_2009_176.nc 1/1_day_2009_177.nc 1/1_day_2009_178.nc 1/1_day_2009_179.nc 1/1_day_2009_180.nc 1/1_day_2009_181.nc 1/1_day_2009_182.nc 1/1_day_2009_183.nc 1/1_day_2009_184.nc 1/1_day_2009_185.nc 1/1_day_2009_186.nc 1/1_day_2009_187.nc 1/1_day_2009_188.nc 1/1_day_2009_189.nc 1/1_day_2009_190.nc 1/1_day_2009_191.nc 1/1_day_2009_192.nc 1/1_day_2009_193.nc 1/1_day_2009_194.nc 1/1_day_2009_195.nc 1/1_day_2009_196.nc 1/1_day_2009_197.nc 1/1_day_2009_198.nc 1/1_day_2009_199.nc 2/1_day_2009_200.nc 2/1_day_2009_201.nc 2/1_day_2009_202.nc 2/1_day_2009_203.nc 2/1_day_2009_204.nc 2/1_day_2009_205.nc 2/1_day_2009_206.nc 2/1_day_2009_207.nc 2/1_day_2009_208.nc 2/1_day_2009_209.nc 2/1_day_2009_210.nc 2/1_day_2009_211.nc 2/1_day_2009_212.nc 2/1_day_2009_213.nc 2/1_day_2009_214.nc 2/1_day_2009_215.nc 2/1_day_2009_216.nc 2/1_day_2009_217.nc 2/1_day_2009_218.nc 2/1_day_2009_219.nc 2/1_day_2009_220.nc 2/1_day_2009_221.nc 2/1_day_2009_222.nc 2/1_day_2009_223.nc 2/1_day_2009_224.nc 2/1_day_2009_225.nc 2/1_day_2009_226.nc 2/1_day_2009_227.nc 2/1_day_2009_228.nc 2/1_day_2009_229.nc 2/1_day_2009_230.nc 2/1_day_2009_231.nc 2/1_day_2009_232.nc 2/1_day_2009_233.nc 2/1_day_2009_234.nc 2/1_day_2009_235.nc 2/1_day_2009_236.nc 2/1_day_2009_237.nc 2/1_day_2009_238.nc 2/1_day_2009_239.nc 2/1_day_2009_240.nc 2/1_day_2009_241.nc 2/1_day_2009_242.nc 2/1_day_2009_243.nc 2/1_day_2009_244.nc 2/1_day_2009_245.nc 2/1_day_2009_246.nc 2/1_day_2009_247.nc 2/1_day_2009_248.nc 2/1_day_2009_249.nc 2/1_day_2009_250.nc 2/1_day_2009_251.nc 2/1_day_2009_252.nc 2/1_day_2009_253.nc 2/1_day_2009_254.nc 2/1_day_2009_255.nc 2/1_day_2009_256.nc 2/1_day_2009_257.nc 2/1_day_2009_258.nc 2/1_day_2009_259.nc 2/1_day_2009_260.nc 2/1_day_2009_261.nc 2/1_day_2009_262.nc 2/1_day_2009_263.nc 2/1_day_2009_264.nc 2/1_day_2009_265.nc 2/1_day_2009_266.nc 2/1_day_2009_267.nc 2/1_day_2009_268.nc 2/1_day_2009_269.nc 2/1_day_2009_270.nc 2/1_day_2009_271.nc 2/1_day_2009_272.nc 2/1_day_2009_273.nc 2/1_day_2009_274.nc 2/1_day_2009_275.nc 2/1_day_2009_276.nc 2/1_day_2009_277.nc 2/1_day_2009_278.nc 2/1_day_2009_279.nc 2/1_day_2009_280.nc 2/1_day_2009_281.nc 2/1_day_2009_282.nc 2/1_day_2009_283.nc 2/1_day_2009_284.nc 2/1_day_2009_285.nc 2/1_day_2009_286.nc 2/1_day_2009_287.nc 2/1_day_2009_288.nc 2/1_day_2009_289.nc 2/1_day_2009_290.nc 2/1_day_2009_291.nc 2/1_day_2009_292.nc 2/1_day_2009_293.nc 2/1_day_2009_294.nc 2/1_day_2009_295.nc 2/1_day_2009_296.nc 2/1_day_2009_297.nc 2/1_day_2009_298.nc 2/1_day_2009_299.nc 3/1_day_2009_300.nc 3/1_day_2009_301.nc 3/1_day_2009_302.nc 3/1_day_2009_303.nc 3/1_day_2009_304.nc 3/1_day_2009_305.nc 3/1_day_2009_306.nc 3/1_day_2009_307.nc 3/1_day_2009_308.nc 3/1_day_2009_309.nc 3/1_day_2009_310.nc 3/1_day_2009_311.nc 3/1_day_2009_312.nc 3/1_day_2009_313.nc 3/1_day_2009_314.nc 3/1_day_2009_315.nc 3/1_day_2009_316.nc 3/1_day_2009_317.nc 3/1_day_2009_318.nc 3/1_day_2009_319.nc 3/1_day_2009_320.nc 3/1_day_2009_321.nc 3/1_day_2009_322.nc 3/1_day_2009_323.nc 3/1_day_2009_324.nc 3/1_day_2009_325.nc 3/1_day_2009_326.nc 3/1_day_2009_327.nc 3/1_day_2009_328.nc 3/1_day_2009_329.nc 3/1_day_2009_330.nc 3/1_day_2009_331.nc 3/1_day_2009_332.nc 3/1_day_2009_333.nc 3/1_day_2009_334.nc 3/1_day_2009_335.nc 3/1_day_2009_336.nc 3/1_day_2009_337.nc 3/1_day_2009_338.nc 3/1_day_2009_339.nc 3/1_day_2009_340.nc 3/1_day_2009_341.nc 3/1_day_2009_342.nc 3/1_day_2009_343.nc 3/1_day_2009_344.nc 3/1_day_2009_345.nc 3/1_day_2009_346.nc 3/1_day_2009_347.nc 3/1_day_2009_348.nc 3/1_day_2009_349.nc 3/1_day_2009_350.nc 3/1_day_2009_351.nc 3/1_day_2009_352.nc 3/1_day_2009_353.nc 3/1_day_2009_354.nc 3/1_day_2009_355.nc 3/1_day_2009_356.nc 3/1_day_2009_357.nc 3/1_day_2009_358.nc 3/1_day_2009_359.nc 3/1_day_2009_360.nc 3/1_day_2009_361.nc 3/1_day_2009_362.nc 3/1_day_2009_363.nc 3/1_day_2009_364.nc 3/1_day_2009_365.nc oscar_countfix_8day.2009.nc4 infoUrl=??? institution=University of Delaware NCO=netCDF Operators version 4.7.6 (Homepage = http://nco.sf.net, Code = https://github.com/nco/nco) Northernmost_Northing=89.70976356050069 sourceUrl=(local files) Southernmost_Northing=-89.96 standard_name_vocabulary=CF Standard Name Table v70 time_coverage_end=2009-12-31T23:59:59Z time_coverage_start=2000-01-01T23:59:59Z Westernmost_Easting=-179.75

Standard Deviations of AVHRR products at 100km rolling 365-day resolution. Averaging performed by NetCDF Operators cdm_data_type=Grid Conventions=COARDS, CF-1.6, ACDD-1.3 Easternmost_Easting=179.72222222222217 geospatial_lat_max=89.49724279835391 geospatial_lat_min=-89.12703703703703 geospatial_lat_resolution=0.925514403292181 geospatial_lat_units=degrees_north geospatial_lon_max=179.72222222222217 geospatial_lon_min=-179.53703703703704 geospatial_lon_resolution=0.9259259259259258 geospatial_lon_units=degrees_east history=Sat Oct 22 18:20:36 2022: ncrcat 0/1_day_2009_001.nc 0/1_day_2009_002.nc 0/1_day_2009_003.nc 0/1_day_2009_004.nc 0/1_day_2009_005.nc 0/1_day_2009_006.nc 0/1_day_2009_007.nc 0/1_day_2009_008.nc 0/1_day_2009_009.nc 0/1_day_2009_010.nc 0/1_day_2009_011.nc 0/1_day_2009_012.nc 0/1_day_2009_013.nc 0/1_day_2009_014.nc 0/1_day_2009_015.nc 0/1_day_2009_016.nc 0/1_day_2009_017.nc 0/1_day_2009_018.nc 0/1_day_2009_019.nc 0/1_day_2009_020.nc 0/1_day_2009_021.nc 0/1_day_2009_022.nc 0/1_day_2009_023.nc 0/1_day_2009_024.nc 0/1_day_2009_025.nc 0/1_day_2009_026.nc 0/1_day_2009_027.nc 0/1_day_2009_028.nc 0/1_day_2009_029.nc 0/1_day_2009_030.nc 0/1_day_2009_031.nc 0/1_day_2009_032.nc 0/1_day_2009_033.nc 0/1_day_2009_034.nc 0/1_day_2009_035.nc 0/1_day_2009_036.nc 0/1_day_2009_037.nc 0/1_day_2009_038.nc 0/1_day_2009_039.nc 0/1_day_2009_040.nc 0/1_day_2009_041.nc 0/1_day_2009_042.nc 0/1_day_2009_043.nc 0/1_day_2009_044.nc 0/1_day_2009_045.nc 0/1_day_2009_046.nc 0/1_day_2009_047.nc 0/1_day_2009_048.nc 0/1_day_2009_049.nc 0/1_day_2009_050.nc 0/1_day_2009_051.nc 0/1_day_2009_052.nc 0/1_day_2009_053.nc 0/1_day_2009_054.nc 0/1_day_2009_055.nc 0/1_day_2009_056.nc 0/1_day_2009_057.nc 0/1_day_2009_058.nc 0/1_day_2009_059.nc 0/1_day_2009_060.nc 0/1_day_2009_061.nc 0/1_day_2009_062.nc 0/1_day_2009_063.nc 0/1_day_2009_064.nc 0/1_day_2009_065.nc 0/1_day_2009_066.nc 0/1_day_2009_067.nc 0/1_day_2009_068.nc 0/1_day_2009_069.nc 0/1_day_2009_070.nc 0/1_day_2009_071.nc 0/1_day_2009_072.nc 0/1_day_2009_073.nc 0/1_day_2009_074.nc 0/1_day_2009_075.nc 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3/1_day_2009_326.nc 3/1_day_2009_327.nc 3/1_day_2009_328.nc 3/1_day_2009_329.nc 3/1_day_2009_330.nc 3/1_day_2009_331.nc 3/1_day_2009_332.nc 3/1_day_2009_333.nc 3/1_day_2009_334.nc 3/1_day_2009_335.nc 3/1_day_2009_336.nc 3/1_day_2009_337.nc 3/1_day_2009_338.nc 3/1_day_2009_339.nc 3/1_day_2009_340.nc 3/1_day_2009_341.nc 3/1_day_2009_342.nc 3/1_day_2009_343.nc 3/1_day_2009_344.nc 3/1_day_2009_345.nc 3/1_day_2009_346.nc 3/1_day_2009_347.nc 3/1_day_2009_348.nc 3/1_day_2009_349.nc 3/1_day_2009_350.nc 3/1_day_2009_351.nc 3/1_day_2009_352.nc 3/1_day_2009_353.nc 3/1_day_2009_354.nc 3/1_day_2009_355.nc 3/1_day_2009_356.nc 3/1_day_2009_357.nc 3/1_day_2009_358.nc 3/1_day_2009_359.nc 3/1_day_2009_360.nc 3/1_day_2009_361.nc 3/1_day_2009_362.nc 3/1_day_2009_363.nc 3/1_day_2009_364.nc 3/1_day_2009_365.nc /lustre/scratch/orb/avhrr/std_dev/100km/365day/avhrr_std_dev_365day_100km_2009.nc4 infoUrl=??? institution=University of Delaware keywords_vocabulary=GCMD Science Keywords NCO=netCDF Operators version 4.7.6 (Homepage = http://nco.sf.net, Code = https://github.com/nco/nco) Northernmost_Northing=89.49724279835391 sourceUrl=(local files) Southernmost_Northing=-89.12703703703703 standard_name_vocabulary=CF Standard Name Table v70 time_coverage_end=2009-12-31T05:00:00Z time_coverage_start=2000-01-01T05:00:00Z Westernmost_Easting=-179.53703703703704

Savannah Conductivity, Temperature, Depth (CTD) - SAV1803 - SAV1803_SAV1803_33 - 2018-03-11 - 25.9122N 81.7992W. Hydrographic Measurements in the Gulf of Mexico. flags: 1 = good; 3 = mean ± 3*standard deviation; 4 = mean ± 5*standard deviation; 9 = missing cdm_altitude_proxy=depth cdm_data_type=Profile cdm_profile_variables=profile, time, latitude, longitude, platform, instrument, instrument1, instrument2, instrument3, instrument4, instrument5, instrument8, instrument10, instrument12, instrument14, instrument15, crs comment=Processing:datcnv_ox_hysteresis_correction = yes; datcnv_ox_tau_correction = yes; filter_low_pass_tc_A = 0.030; filter_low_pass_tc_B = 0.150; filter_low_pass_A_vars = CStarAt0 CStarTr0, par, dz/dtM; filter_low_pass_B_vars = prDM ;alignctd_adv = c0S/m 0.073, c1S/m 0.073, sbeox0ML/L 3.500, oxsatML/L 3.500; celltm_alpha = 0.0300, 0.0300; celltm_tau = 7.0000, 7.0000; loopedit_minVelocity = 0.010; loopedit_surfaceSoak = 1: minDepth = 0.5, maxDepth = 2; useDeckPress = 1; loopedit_excl_bad_scans = yes comment1=flags: 1 = good; 3 = mean ± 3*standard deviation; 4 = mean ± 5*standard deviation; 9 = missing contributor_country=USA contributor_role_vocabulary=https://vocab.nerc.ac.uk/collection/G04/current/ Conventions=CF-1.6, ACDD-1.3, IOOS-1.2, COARDS Country=USA date_metadata_modified=2023-01-29T11:59:42Z Easternmost_Easting=-81.79916666666666 featureType=Profile geospatial_bounds=POLYGON ((24.00 -83.00, 26.00, -83.00, 26.00, -80.00, 24.00 -80.00, 24.00 -83.00)) geospatial_bounds_crs=EPSG:4326 geospatial_bounds_vertical_crs=EPSG:5831 geospatial_lat_max=25.912166666666668 geospatial_lat_min=25.912166666666668 geospatial_lat_units=degrees_north geospatial_lon_max=-81.79916666666666 geospatial_lon_min=-81.79916666666666 geospatial_lon_units=degrees_east geospatial_vertical_max=8.284 geospatial_vertical_min=1.9 geospatial_vertical_positive=down geospatial_vertical_resolution=0.001581553154058809 geospatial_vertical_units=m grid_mapping_FillValue=-999 grid_mapping_epsg_code=EPSG:4326 grid_mapping_inverse_flattening=298.257223563 grid_mapping_long_name=grid mapping variable for horizontal spatial coordinate reference system (CRS) grid_mapping_longitude_of_prime_meridian=0.0 grid_mapping_missing_value=-999.0 grid_mapping_name=latitude_longitude grid_mapping_semi_major_axis=6378137.0 grid_mapping_standard_name_url=http://mmisw.org/ont/cf/parameter/unknown history=2023-01-29T11:57:21Z id=SAV1803 infoUrl=https://www.aoml.noaa.gov/phod/sfp/index.php institution=NOAA's Atlantic Oceanographic and Meteorological Laboratory/Ocean Chemistry and Ecosystems Division instrument=CTD Sea-Bird SBE-911plus instrument_vocabulary=GCMD Science Keywords Version 9.1.5 keywords_vocabulary=GCMD Science Keywords metadata_link=https://gcoos5.geos.tamu.edu/erddap/tabledap/Walton-Smith_SAV1803_SAV1803_SAV1803_33.html naming_authority=aoml.noaa.gov Northernmost_Northing=25.912166666666668 platform=RV_Savannah platform_name=RV_Savannah platform_vocabulary=https://mmisw.org/ont/ioos/platform processing_level=Geophysical units from raw data program=Florida Keys Monitoring program project=Marine Biodiversity Observation Network references=https://ocean.floridamarine.org/FKNMS_WQPP/ sea_name=Gulf of Mexico source=Rolling Deck to Repository (R2R) Program sourceUrl=(local files) Southernmost_Northing=25.912166666666668 standard_name_vocabulary=CF Standard Name Table v72 station_name=SAV1803_SAV1803_33 subsetVariables=profile, time, latitude, longitude, platform, instrument, instrument1, instrument2, instrument3, instrument4, instrument5, instrument8, instrument10, instrument12, instrument14, instrument15, crs time_coverage_duration=P00Y0M00DT00H00M00S time_coverage_end=2018-03-11T17:31:46Z time_coverage_start=2018-03-11T17:31:46Z Westernmost_Easting=-81.79916666666666

BackgroundRecently, artificial intelligence (AI)-based applications for chest imaging have emerged as potential tools to assist clinicians in the diagnosis and management of patients with coronavirus disease 2019 (COVID-19).ObjectivesTo develop a deep learning-based clinical decision support system for automatic diagnosis of COVID-19 on chest CT scans. Secondarily, to develop a complementary segmentation tool to assess the extent of lung involvement and measure disease severity.MethodsThe Imaging COVID-19 AI initiative was formed to conduct a retrospective multicentre cohort study including 20 institutions from seven different European countries. Patients with suspected or known COVID-19 who underwent a chest CT were included. The dataset was split on the institution-level to allow external evaluation. Data annotation was performed by 34 radiologists/radiology residents and included quality control measures. A multi-class classification model was created using a custom 3D convolutional neural network. For the segmentation task, a UNET-like architecture with a backbone Residual Network (ResNet-34) was selected.ResultsA total of 2,802 CT scans were included (2,667 unique patients, mean [standard deviation] age = 64.6 [16.2] years, male/female ratio 1.3:1). The distribution of classes (COVID-19/Other type of pulmonary infection/No imaging signs of infection) was 1,490 (53.2%), 402 (14.3%), and 910 (32.5%), respectively. On the external test dataset, the diagnostic multiclassification model yielded high micro-average and macro-average AUC values (0.93 and 0.91, respectively). The model provided the likelihood of COVID-19 vs other cases with a sensitivity of 87% and a specificity of 94%. The segmentation performance was moderate with Dice similarity coefficient (DSC) of 0.59. An imaging analysis pipeline was developed that returned a quantitative report to the user.ConclusionWe developed a deep learning-based clinical decision support system that could become an efficient concurrent reading tool to assist clinicians, utilising a newly created European dataset including more than 2,800 CT scans.

The automatic cutting of coal and rock surface morphology modeling based on the actual geological environment of coal mine underground excavation and mining is of great significance for improving the surface quality of coal and rock after cutting and enhancing the safety and stability of advanced support. To this end, using the principle of coordinate transformation, the kinematic trajectory of the cutting head of the tunneling machine is established, and the contour morphology of the cutting head under variable cutting technology is obtained. Then, based on the regenerative vibration theory of the cutting head, a dynamic model of the cutting head coal wall is established, and the coordinate relationship of the cutting head in the tunnel coordinate system under vibration induction is analyzed. Based on fractal theory and Z-MAP method, a simulation method for the surface morphology of coal and rock after cutting is proposed, which is driven by the cutting trajectory Under the coupling effect of cutting vibration induction and random fragmentation of coal and rock, simulation of the surface morphology of comprehensive excavation tunnels was conducted, and relevant experiments were conducted to verify the results. A 1:3 similarity experimental model of EBZ160 tunneling machine was used to build a cutting head coal and rock system cutting experimental platform for comparative experiments of cutting morphology. Furthermore, statistical methods were used to compare and evaluate the simulated roof with the actual roof. The results show that the relative errors between the maximum range of peaks and valleys, the peak skewness coefficient of height standard deviation, and the kurtosis coefficient of the actual roof are 1.3%, 24.5%, 16%, and 2.9%, respectively. Overall, this indicates that the surface morphology distribution characteristics of the simulated roof and the actual roof are similar, verifying the effectiveness of the modeling and simulation method proposed in this paper, and providing theoretical support for the design and optimization of advanced support in the future.

Standard Deviations of SeaWIFS products at 100km rolling 30-day resolution. Averaging performed by NetCDF Operators cdm_data_type=Grid Conventions=COARDS, CF-1.6, ACDD-1.3 Easternmost_Easting=179.72222222222217 geospatial_lat_max=89.49724279835391 geospatial_lat_min=-89.12703703703703 geospatial_lat_resolution=0.925514403292181 geospatial_lat_units=degrees_north geospatial_lon_max=179.72222222222217 geospatial_lon_min=-179.53703703703704 geospatial_lon_resolution=0.9259259259259258 geospatial_lon_units=degrees_east history=Sat Oct 29 06:56:23 2022: ncrcat 0/1_day_2000_001.nc 0/1_day_2000_002.nc 0/1_day_2000_003.nc 0/1_day_2000_004.nc 0/1_day_2000_005.nc 0/1_day_2000_006.nc 0/1_day_2000_007.nc 0/1_day_2000_008.nc 0/1_day_2000_009.nc 0/1_day_2000_010.nc 0/1_day_2000_011.nc 0/1_day_2000_012.nc 0/1_day_2000_013.nc 0/1_day_2000_014.nc 0/1_day_2000_015.nc 0/1_day_2000_016.nc 0/1_day_2000_017.nc 0/1_day_2000_018.nc 0/1_day_2000_019.nc 0/1_day_2000_020.nc 0/1_day_2000_021.nc 0/1_day_2000_022.nc 0/1_day_2000_023.nc 0/1_day_2000_024.nc 0/1_day_2000_025.nc 0/1_day_2000_026.nc 0/1_day_2000_027.nc 0/1_day_2000_028.nc 0/1_day_2000_029.nc 0/1_day_2000_030.nc 0/1_day_2000_031.nc 0/1_day_2000_032.nc 0/1_day_2000_033.nc 0/1_day_2000_034.nc 0/1_day_2000_035.nc 0/1_day_2000_036.nc 0/1_day_2000_037.nc 0/1_day_2000_038.nc 0/1_day_2000_039.nc 0/1_day_2000_040.nc 0/1_day_2000_041.nc 0/1_day_2000_042.nc 0/1_day_2000_043.nc 0/1_day_2000_044.nc 0/1_day_2000_045.nc 0/1_day_2000_046.nc 0/1_day_2000_047.nc 0/1_day_2000_048.nc 0/1_day_2000_049.nc 0/1_day_2000_050.nc 0/1_day_2000_051.nc 0/1_day_2000_052.nc 0/1_day_2000_053.nc 0/1_day_2000_054.nc 0/1_day_2000_055.nc 0/1_day_2000_056.nc 0/1_day_2000_057.nc 0/1_day_2000_058.nc 0/1_day_2000_059.nc 0/1_day_2000_060.nc 0/1_day_2000_061.nc 0/1_day_2000_062.nc 0/1_day_2000_063.nc 0/1_day_2000_064.nc 0/1_day_2000_065.nc 0/1_day_2000_066.nc 0/1_day_2000_067.nc 0/1_day_2000_068.nc 0/1_day_2000_069.nc 0/1_day_2000_070.nc 0/1_day_2000_071.nc 0/1_day_2000_072.nc 0/1_day_2000_073.nc 0/1_day_2000_074.nc 0/1_day_2000_075.nc 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2/1_day_2000_276.nc 2/1_day_2000_277.nc 2/1_day_2000_278.nc 2/1_day_2000_279.nc 2/1_day_2000_280.nc 2/1_day_2000_281.nc 2/1_day_2000_282.nc 2/1_day_2000_283.nc 2/1_day_2000_284.nc 2/1_day_2000_285.nc 2/1_day_2000_286.nc 2/1_day_2000_287.nc 2/1_day_2000_288.nc 2/1_day_2000_289.nc 2/1_day_2000_290.nc 2/1_day_2000_291.nc 2/1_day_2000_292.nc 2/1_day_2000_293.nc 2/1_day_2000_294.nc 2/1_day_2000_295.nc 2/1_day_2000_296.nc 2/1_day_2000_297.nc 2/1_day_2000_298.nc 2/1_day_2000_299.nc 3/1_day_2000_300.nc 3/1_day_2000_301.nc 3/1_day_2000_302.nc 3/1_day_2000_303.nc 3/1_day_2000_304.nc 3/1_day_2000_305.nc 3/1_day_2000_306.nc 3/1_day_2000_307.nc 3/1_day_2000_308.nc 3/1_day_2000_309.nc 3/1_day_2000_310.nc 3/1_day_2000_311.nc 3/1_day_2000_312.nc 3/1_day_2000_313.nc 3/1_day_2000_314.nc 3/1_day_2000_315.nc 3/1_day_2000_316.nc 3/1_day_2000_317.nc 3/1_day_2000_318.nc 3/1_day_2000_319.nc 3/1_day_2000_320.nc 3/1_day_2000_321.nc 3/1_day_2000_322.nc 3/1_day_2000_323.nc 3/1_day_2000_324.nc 3/1_day_2000_325.nc 3/1_day_2000_326.nc 3/1_day_2000_327.nc 3/1_day_2000_328.nc 3/1_day_2000_329.nc 3/1_day_2000_330.nc 3/1_day_2000_331.nc 3/1_day_2000_332.nc 3/1_day_2000_333.nc 3/1_day_2000_334.nc 3/1_day_2000_335.nc 3/1_day_2000_336.nc 3/1_day_2000_337.nc 3/1_day_2000_338.nc 3/1_day_2000_339.nc 3/1_day_2000_340.nc 3/1_day_2000_341.nc 3/1_day_2000_342.nc 3/1_day_2000_343.nc 3/1_day_2000_344.nc 3/1_day_2000_345.nc 3/1_day_2000_346.nc 3/1_day_2000_347.nc 3/1_day_2000_348.nc 3/1_day_2000_349.nc 3/1_day_2000_350.nc 3/1_day_2000_351.nc 3/1_day_2000_352.nc 3/1_day_2000_353.nc 3/1_day_2000_354.nc 3/1_day_2000_355.nc 3/1_day_2000_356.nc 3/1_day_2000_357.nc 3/1_day_2000_358.nc 3/1_day_2000_359.nc 3/1_day_2000_360.nc 3/1_day_2000_361.nc 3/1_day_2000_362.nc 3/1_day_2000_363.nc 3/1_day_2000_364.nc 3/1_day_2000_365.nc /lustre/scratch/orb/seawifs/std_dev/100km/30day/seawifs_std_dev_30day_100km_2000.nc4 infoUrl=??? institution=University of Delaware NCO=netCDF Operators version 4.7.6 (Homepage = http://nco.sf.net, Code = https://github.com/nco/nco) Northernmost_Northing=89.49724279835391 sourceUrl=(local files) Southernmost_Northing=-89.12703703703703 standard_name_vocabulary=CF Standard Name Table v70 time_coverage_end=2009-12-31T05:00:00Z time_coverage_start=2000-01-01T05:00:00Z Westernmost_Easting=-179.53703703703704

Standard Deviations of SeaWIFS products at 50km rolling 8-day resolution. Averaging performed by NetCDF Operators cdm_data_type=Grid Conventions=COARDS, CF-1.6, ACDD-1.3 Easternmost_Easting=179.95370370370364 geospatial_lat_max=89.72862139917694 geospatial_lat_min=-89.82117283950616 geospatial_lat_resolution=0.46275720164609047 geospatial_lat_units=degrees_north geospatial_lon_max=179.95370370370364 geospatial_lon_min=-179.7685185185185 geospatial_lon_resolution=0.4629629629629629 geospatial_lon_units=degrees_east history=Thu Dec 15 10:21:37 2022: ncrcat 0/1_day_2003_001.nc 0/1_day_2003_002.nc 0/1_day_2003_003.nc 0/1_day_2003_004.nc 0/1_day_2003_005.nc 0/1_day_2003_006.nc 0/1_day_2003_007.nc 0/1_day_2003_008.nc 0/1_day_2003_009.nc 0/1_day_2003_010.nc 0/1_day_2003_011.nc 0/1_day_2003_012.nc 0/1_day_2003_013.nc 0/1_day_2003_014.nc 0/1_day_2003_015.nc 0/1_day_2003_016.nc 0/1_day_2003_017.nc 0/1_day_2003_018.nc 0/1_day_2003_019.nc 0/1_day_2003_020.nc 0/1_day_2003_021.nc 0/1_day_2003_022.nc 0/1_day_2003_023.nc 0/1_day_2003_024.nc 0/1_day_2003_025.nc 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3/1_day_2003_326.nc 3/1_day_2003_327.nc 3/1_day_2003_328.nc 3/1_day_2003_329.nc 3/1_day_2003_330.nc 3/1_day_2003_331.nc 3/1_day_2003_332.nc 3/1_day_2003_333.nc 3/1_day_2003_334.nc 3/1_day_2003_335.nc 3/1_day_2003_336.nc 3/1_day_2003_337.nc 3/1_day_2003_338.nc 3/1_day_2003_339.nc 3/1_day_2003_340.nc 3/1_day_2003_341.nc 3/1_day_2003_342.nc 3/1_day_2003_343.nc 3/1_day_2003_344.nc 3/1_day_2003_345.nc 3/1_day_2003_346.nc 3/1_day_2003_347.nc 3/1_day_2003_348.nc 3/1_day_2003_349.nc 3/1_day_2003_350.nc 3/1_day_2003_351.nc 3/1_day_2003_352.nc 3/1_day_2003_353.nc 3/1_day_2003_354.nc 3/1_day_2003_355.nc 3/1_day_2003_356.nc 3/1_day_2003_357.nc 3/1_day_2003_358.nc 3/1_day_2003_359.nc 3/1_day_2003_360.nc 3/1_day_2003_361.nc 3/1_day_2003_362.nc /lustre/scratch/orb/seawifs/std_dev/50km/8day/seawifs_50km_std_dev_8day_2003.nc4 infoUrl=??? institution=University of Delaware NCO=netCDF Operators version 4.7.6 (Homepage = http://nco.sf.net, Code = https://github.com/nco/nco) Northernmost_Northing=89.72862139917694 sourceUrl=(local files) Southernmost_Northing=-89.82117283950616 standard_name_vocabulary=CF Standard Name Table v70 time_coverage_end=2010-12-11T05:00:00Z time_coverage_start=2000-01-01T05:00:00Z Westernmost_Easting=-179.7685185185185

Standard Deviations of MODIS AQUA products at 100km rolling 8-day resolution. Averaging performed by NetCDF Operators cdm_data_type=Grid Conventions=COARDS, CF-1.6, ACDD-1.3 Easternmost_Easting=179.72222222222217 geospatial_lat_max=89.49724279835391 geospatial_lat_min=-89.12703703703703 geospatial_lat_resolution=0.925514403292181 geospatial_lat_units=degrees_north geospatial_lon_max=179.72222222222217 geospatial_lon_min=-179.53703703703704 geospatial_lon_resolution=0.9259259259259258 geospatial_lon_units=degrees_east history=Sat Oct 1 11:15:18 2022: ncrcat 2005/0/1_day_2005_001.nc 2005/0/1_day_2005_002.nc 2005/0/1_day_2005_003.nc 2005/0/1_day_2005_004.nc 2005/0/1_day_2005_005.nc 2005/0/1_day_2005_006.nc 2005/0/1_day_2005_007.nc 2005/0/1_day_2005_008.nc 2005/0/1_day_2005_009.nc 2005/0/1_day_2005_010.nc 2005/0/1_day_2005_011.nc 2005/0/1_day_2005_012.nc 2005/0/1_day_2005_013.nc 2005/0/1_day_2005_014.nc 2005/0/1_day_2005_015.nc 2005/0/1_day_2005_016.nc 2005/0/1_day_2005_017.nc 2005/0/1_day_2005_018.nc 2005/0/1_day_2005_019.nc 2005/0/1_day_2005_020.nc 2005/0/1_day_2005_021.nc 2005/0/1_day_2005_022.nc 2005/0/1_day_2005_023.nc 2005/0/1_day_2005_024.nc 2005/0/1_day_2005_025.nc 2005/0/1_day_2005_026.nc 2005/0/1_day_2005_027.nc 2005/0/1_day_2005_028.nc 2005/0/1_day_2005_029.nc 2005/0/1_day_2005_030.nc 2005/0/1_day_2005_031.nc 2005/0/1_day_2005_032.nc 2005/0/1_day_2005_033.nc 2005/0/1_day_2005_034.nc 2005/0/1_day_2005_035.nc 2005/0/1_day_2005_036.nc 2005/0/1_day_2005_037.nc 2005/0/1_day_2005_038.nc 2005/0/1_day_2005_039.nc 2005/0/1_day_2005_040.nc 2005/0/1_day_2005_041.nc 2005/0/1_day_2005_042.nc 2005/0/1_day_2005_043.nc 2005/0/1_day_2005_044.nc 2005/0/1_day_2005_045.nc 2005/0/1_day_2005_046.nc 2005/0/1_day_2005_047.nc 2005/0/1_day_2005_048.nc 2005/0/1_day_2005_049.nc 2005/0/1_day_2005_050.nc 2005/0/1_day_2005_051.nc 2005/0/1_day_2005_052.nc 2005/0/1_day_2005_053.nc 2005/0/1_day_2005_054.nc 2005/0/1_day_2005_055.nc 2005/0/1_day_2005_056.nc 2005/0/1_day_2005_057.nc 2005/0/1_day_2005_058.nc 2005/0/1_day_2005_059.nc 2005/0/1_day_2005_060.nc 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2005/3/1_day_2005_341.nc 2005/3/1_day_2005_342.nc 2005/3/1_day_2005_343.nc 2005/3/1_day_2005_344.nc 2005/3/1_day_2005_345.nc 2005/3/1_day_2005_346.nc 2005/3/1_day_2005_347.nc 2005/3/1_day_2005_348.nc 2005/3/1_day_2005_349.nc 2005/3/1_day_2005_350.nc 2005/3/1_day_2005_351.nc 2005/3/1_day_2005_352.nc 2005/3/1_day_2005_353.nc 2005/3/1_day_2005_354.nc 2005/3/1_day_2005_355.nc 2005/3/1_day_2005_356.nc 2005/3/1_day_2005_357.nc 2005/3/1_day_2005_358.nc 2005/3/1_day_2005_359.nc 2005/3/1_day_2005_360.nc 2005/3/1_day_2005_361.nc 2005/3/1_day_2005_362.nc 2005/3/1_day_2005_363.nc 2005/3/1_day_2005_364.nc 2005/3/1_day_2005_365.nc /lustre/scratch/orb/aqua/std_dev/100km/8day/aqua_8day_stddev.2005.nc4 infoUrl=??? institution=University of Delaware keywords_vocabulary=GCMD Science Keywords NCO=netCDF Operators version 4.7.6 (Homepage = http://nco.sf.net, Code =

Walton-Smith Conductivity, Temperature, Depth (CTD) - WS17086 - WS17086_WS17086Stn57.3 - 2017-03-29 - 25.3532N 81.6515W. Hydrographic Measurements in the Gulf of Mexico. flags: 1 = good; 3 = mean ± 3*standard deviation; 4 = mean ± 5*standard deviation; 9 = missing. other acknowledgement=other cdm_altitude_proxy=depth cdm_data_type=Profile cdm_profile_variables=profile, time, latitude, longitude, platform, instrument, instrument1, instrument2, instrument3, instrument4, instrument5, instrument6, instrument8, instrument9, instrument10, instrument11, instrument16, crs comment=Processing:datcnv_ox_hysteresis_correction = yes; datcnv_ox_tau_correction = yes; filter_low_pass_tc_A = 0.030; filter_low_pass_tc_B = 0.150; filter_low_pass_A_vars = CStarAt0 CStarTr0, par, dz/dtM; filter_low_pass_B_vars = prDM ;alignctd_adv = c0S/m 0.073, c1S/m 0.073, sbeox0ML/L 3.500, oxsatML/L 3.500; celltm_alpha = 0.0300, 0.0300; celltm_tau = 7.0000, 7.0000; loopedit_minVelocity = 0.010; loopedit_surfaceSoak = 1: minDepth = 0.5, maxDepth = 2; useDeckPress = 1; loopedit_excl_bad_scans = yes comment1=flags: 1 = good; 3 = mean ± 3*standard deviation; 4 = mean ± 5*standard deviation; 9 = missing comment2=other contributor_country=USA contributor_email=other contributor_institution=other contributor_name=other contributor_phone=other contributor_role=other contributor_role_vocabulary=https://vocab.nerc.ac.uk/collection/G04/current/ contributor_url=other Conventions=CF-1.10, ACDD-1.3, IOOS-1.2, COARDS Country=USA date_metadata_modified=2024-05-17T13:58:09Z Easternmost_Easting=-81.6515 featureType=Profile geospatial_bounds=POLYGON ((24.00 -83.00, 26.00, -83.00, 26.00, -80.00, 24.00 -80.00, 24.00 -83.00)) geospatial_bounds_crs=EPSG:4326 geospatial_bounds_vertical_crs=EPSG:5831 geospatial_lat_max=25.353166666666667 geospatial_lat_min=25.353166666666667 geospatial_lat_units=degrees_north geospatial_lon_max=-81.6515 geospatial_lon_min=-81.6515 geospatial_lon_units=degrees_east geospatial_vertical_max=11.412 geospatial_vertical_min=1.844 geospatial_vertical_positive=down geospatial_vertical_resolution=0.00623778071334214 geospatial_vertical_units=m grid_mapping_FillValue=-999 grid_mapping_epsg_code=EPSG:4326 grid_mapping_inverse_flattening=298.257223563 grid_mapping_long_name=grid mapping variable for horizontal spatial coordinate reference system (CRS) grid_mapping_longitude_of_prime_meridian=0.0 grid_mapping_missing_value=-999.0 grid_mapping_name=latitude_longitude grid_mapping_semi_major_axis=6378137.0 grid_mapping_standard_name_url=http://mmisw.org/ont/cf/parameter/other grid_mapping_units=other history=2024-05-17T13:42:50Z id=WS17086 infoUrl=https://www.aoml.noaa.gov/phod/sfp/index.php institution=NOAA's Atlantic Oceanographic and Meteorological Laboratory/Ocean Chemistry and Ecosystems Division instrument=CTD Sea-Bird SBE-911plus instrument_vocabulary=GCMD Science Keywords Version 9.1.5 keywords_vocabulary=GCMD Science Keywords metadata_link=https://gcoos5.geos.tamu.edu/erddap/tabledap/Walton-Smith_WS17086_WS17086_WS17086Stn57.3.html naming_authority=aoml.noaa.gov Northernmost_Northing=25.353166666666667 platform=RV_Weatherbird_II platform_id=other platform_name=RV_Weatherbird_II platform_vocabulary=https://mmisw.org/ont/ioos/platform processing_level=Geophysical units from raw data program=Florida Keys Monitoring program project=Marine Biodiversity Observation Network references=https://ocean.floridamarine.org/FKNMS_WQPP/ sea_name=Gulf of Mexico source=Rolling Deck to Repository (R2R) Program sourceUrl=(local files) Southernmost_Northing=25.353166666666667 standard_name_vocabulary=CF Standard Name Table v72 station_name=WS17086_WS17086Stn57.3 subsetVariables=profile, time, latitude, longitude, platform, instrument, instrument1, instrument2, instrument3, instrument4, instrument5, instrument6, instrument8, instrument9, instrument10, instrument11, instrument16, crs time_coverage_duration=P00Y0M00DT00H00M00S time_coverage_end=2017-03-29T14:22:24Z time_coverage_resolution=other time_coverage_start=2017-03-29T14:22:24Z Westernmost_Easting=-81.6515

RV_FG_Walton_Smith cruise WS21093 in 2021. Hydrographic Measurements in the Gulf of Mexico. flags: 1 = good; 3 = mean ± 3*standard deviation; 4 = mean ± 5*standard deviation; 9 = missing cdm_altitude_proxy=depth cdm_data_type=Profile cdm_profile_variables=profile comment=Processing:datcnv_ox_hysteresis_correction = no; datcnv_ox_tau_correction = yes; filter_low_pass_tc_A = 0.030; filter_low_pass_tc_B = 0.150; filter_low_pass_A_vars = ; filter_low_pass_B_vars = prDM ;alignctd_adv = c0S/m 0.073, c1S/m 0.073, sbeox0ML/L 3.500, oxsatML/L 3.500; celltm_alpha = 0.0300, 0.0300; celltm_tau = 7.0000, 7.0000; loopedit_minVelocity = 0.010; loopedit_surfaceSoak: minDepth = 0.5, maxDepth = 2; useDeckPress = 1; loopedit_excl_bad_scans = no comment1=flags: 1 = good; 3 = mean ± 3*standard deviation; 4 = mean ± 5*standard deviation; 9 = missing contributor_country=USA contributor_role_vocabulary=https://vocab.nerc.ac.uk/collection/G04/current/ Conventions=CF-1.6, ACDD-1.3, IOOS-1.2, COARDS Country=USA date_metadata_modified=2021-09-09T15:48:52Z Easternmost_Easting=-83.30033333333333 featureType=Profile geospatial_bounds=POLYGON ((24.00 -83.00, 26.00, -83.00, 26.00, -80.00, 24.00 -80.00, 24.00 -83.00)) geospatial_bounds_crs=EPSG:4326 geospatial_bounds_vertical_crs=EPSG:5831 geospatial_lat_max=27.616833333333332 geospatial_lat_min=27.616833333333332 geospatial_lat_units=degrees_north geospatial_lon_max=-83.30033333333333 geospatial_lon_min=-83.30033333333333 geospatial_lon_units=degrees_east geospatial_vertical_max=31.314 geospatial_vertical_min=2.743 geospatial_vertical_positive=down geospatial_vertical_resolution=0.005225895825637237 geospatial_vertical_units=m history=2021-09-09T15:39:41Z id=WS21093 infoUrl=https://www.aoml.noaa.gov/phod/sfp/index.php institution=NOAA AOML/OCED instrument=CTD Sea-Bird SBE-911plus instrument_vocabulary=GCMD Science Keywords Version 9.1.5 keywords_vocabulary=GCMD Science Keywords metadata_link=https://gcoos5.geos.tamu.edu/erddap/tabledap/WS21093_STN.TB5.html naming_authority=aoml.noaa.gov Northernmost_Northing=27.616833333333332 platform=RV_FG_Walton_Smith platform_name=RV_FG_Walton_Smith platform_vocabulary=https://mmisw.org/ont/ioos/platform processing_level=Geophysical units from raw data program=Florida Keys Monitoring program project=Marine Biodiversity Observation Network references=https://ocean.floridamarine.org/FKNMS_WQPP/ sea_name=Gulf of Mexico source=Rolling Deck to Repository (R2R) Program sourceUrl=(local files) Southernmost_Northing=27.616833333333332 standard_name_vocabulary=CF Standard Name Table v72 station_name=WS21093_STN.TB5 subsetVariables=profile, time, latitude, longitude, sea_water_pressure_qc, sea_water_temperature_qc, sea_water_temperature2_qc, surface_photosynthetically_available_radiation_qc, altimeter_qc, depth_qc, descent_rate, descent_rate_qc, sound_velocity_qc, platform, instrument, instrument1, instrument2, instrument3, instrument4, instrument5, instrument6, instrument7, instrument8, instrument9, instrument10, instrument11, crs time_coverage_duration=P00Y0M00DT00H00M00S time_coverage_end=2021-04-07T13:14:56Z time_coverage_start=2021-04-07T13:14:56Z Westernmost_Easting=-83.30033333333333