In 2022, around ** percent of respondents in the United States have stated that their breakups tended to be messy and dramatic. In comparison, around ** percent of respondents claimed that their breakups tended to be casual and civil.

In 2022, around ** percent of respondents in the United States have been broken up with in person, compared to ** percent by a phone call and ** percent by text.

In 2022, around ** percent of men and ** percent of women in the United States have stated that they have broken up a relationship. In comparison around ** percent of men and ** percent of women claimed that a former partner has broken up with them.

This statistic shows the results of a survey conducted in the United States in 2019 about breaking up via text message. Some 11 percent of respondents stated that they had broken up with someone via text message (e.g. WhatsApp, SMS), email or social media message more than one time.

The Tanana river in the Interior of Alaska usually freezes over during October and November. The ice continues to grow throughout the winter accumulating an average maximum thickness of about 110 cm, depending upon winter weather conditions.The Nenana Ice Classic competition began in 1917 when railroad engineers bet a total of 800 dollars, winner takes all, guessing the exact time (month, day, hour, minute) ice on the Tanana River would break up. Each year since then, Alaska residents have guessed at the timing of the river breakup. A tripod, connected to an on-shore clock with a string, is planted in two feet of river ice during river freeze-up in October or November. The following spring, the clock automatically stops when the tripod moves as the ice breaks up. The time on the clock is used as the river ice breakup time.Many factors influence the river ice breakup, such as air temperature, ice thickness, snow cover, wind, water temperature, and depth of water below the ice. Generally, the Tanana river ice breaks up in late April or early May (historically, April 20 to May 20). The time series of Tanana river ice breakup dates can be used to indicate climate change in the region.

Raw experimental data (Approach Avoidance Task- Excel file). Survey data and processed experimental data (summary Approach Avoidance Task measures - SPSS Data file). Syntax for analyses reported in the paper (SPSS Syntax file). Submitted paper (methods and results contain details on data collection and data analysis)

Many social groups are made up of complex social networks in which each individual tends to associate with a distinct subset of its groupmates. If social groups increase in size over time, competition often leads to permanent group fission. During such fissions, complex social networks present both a collective decision problem and a multidimensional optimization problem: it is advantageous for each individual to remain with their closest allies after a fission, but impossible for every individual to do so. Here, we develop computational algorithms designed to simulate group fissions in a network theoretic framework. We focus on three fission algorithms ("democracy" "community," and "despotism") that fall on a spectrum from a democratic to a dictatorial collective decision. We parameterize our social networks with data from baboons (Papio cynocephalus) and compare our simulated fissions with actual baboon fission events. We find that the democracy and community algorithms (i.e., egalitarian decisions where each individual influences the outcome) better maintain social networks during simulated fissions than despotic decisions (those driven primarily by a single individual). We also find that egalitarian decisions are good at predicting the observed individual-level outcomes of observed fissions, although the observed fissions often disturbed their social networks more than the simulated egalitarian fissions. ... [Read More]

Ice breakup dates of Chequamegon Bay, Lake Superior from 1911 to 2022 were compiled by Lori Evrard (USGS, GLSC, Lake Superior Biological Station, Ashland, WI). Ice breakup date is the day in spring when winter ice cover substantially leaves a water body. Local residents deem "ice breakup" as when the ice moves northeast of a line straight across Chequamegon Bay out from Ellis Avenue (State highway 13). Another way ice breakup was determined has been if you could drive a boat from the outlet of Fish Creek to Houghton Point. The ice may move back and forth over that line but the ice is breaking up, moving and melting from that date on. Ellis Avenue ends on a bluff (46.5925 degrees North, 90.8827 degrees West) that provides a clear view of Chequamegon Bay from Fish Creek to Houghton Point. Mrs. C. J. Hoskings recorded the dates from 1911 to 1980. Mr. LeRoy C. Margenau recorded the dates from 1981 to 1991. The Ashland Marina recorded the dates from 1992-1999 and 2001. Lori Evrard (USGS) recorded dates after 1999 except 2001. USGS converted each date to a consecutive day of the year value. The date of ice breakup will be updated annually to append that year's date.

The permanent breakup of 2019

Vietnam Exports of vessels and other floating structures for breaking up to Portugal was US$3.37 Million during 2013, according to the United Nations COMTRADE database on international trade. Vietnam Exports of vessels and other floating structures for breaking up to Portugal - data, historical chart and statistics - was last updated on May of 2025.

This dataset contains the data output necessary to reproduce the figures in the paper, Aiyer, A. and C. Meneveau (2020). Most data are contained in compressed python files with an accompanying load/read script. Documentation in the read script specifies variable names. A dataset description document gives an overview of the data, including units. The data is generated from a 1D ODE model and from large eddy simulations (LES). The LES data consist of first-order velocity and concentration statistics and the droplet size distribution. The radial and axial distributions and the variability of key quantities such as the Sauter mean diameter, total surface area and droplet breakup time-scale were quantified and their sensitivity to the Weber number were explored. This dataset supports the publication: Aiyer, A., & Meneveau, C. (2020). Coupled population balance and large eddy simulation model for polydisperse droplet evolution in a turbulent round jet. Physical Review Fluids, 5(11). doi:10.1103/physrevfluids.5.114305.

Ice breakup dates of Chequamegon Bay, Lake Superior from 1911 to 2020 were compiled by Lori Evrard (USGS, GLSC, Lake Superior Biological Station, Ashland, WI). Ice breakup date is the day in spring when winter ice cover substantially leaves a water body. Local residents deem "ice breakup" as when the ice moves northeast of a line straight across Chequamegon Bay out from Ellis Avenue (State highway 13). Another way ice breakup was determined has been if you could drive a boat from the outlet of Fish Creek to Houghton Point. The ice may move back and forth over that line but the ice is breaking up, moving and melting from that date on. Ellis Avenue ends on a bluff (46.5925 degrees North, 90.8827 degrees West) that provides a clear view of Chequamegon Bay from Fish Creek to Houghton Point. Mrs. C. J. Hoskings recorded the dates from 1911 to 1980. Mr. LeRoy C. Margenau recorded the dates from 1981 to 1991. The Ashland Marina recorded the dates from 1992-1999 and 2001. Lori Evrard (USGS) recorded dates after 1999 except 2001. USGS converted the dates to Julian dates. The date of ice breakup will be updated annually to append that year's date.

The dataset includes the drawings of the air swirlers, non-dimensional breakup lengths, first droplet locations, vector fields of the annular air flows, vorticity maps, POD modes, frequencies of the flapping instabilities, and 2D spectra.

This statistic shows the share of Americans who would leave their partner if they wanted an open relationship. During the survey, conducted in March 2016, 46 percent of the men interviewed stated they would leave their romantic partner if they were to deal with such a request. 67 percent of the female respondents stated the same.

Events of complete destruction of target: more then 4 protons with momenta from 0.15 to 0.75 GeV/c.

Here we present thermochronology data from sedimentary rock samples of late Cretaceous to Paleogene age with unusually high thermal maturities from eastern North Greenland and western Svalbard. The data are interpreted and discussed in the article "Shallow Thermal Anomalies and their Role in the Breakup Evolution along the Conjugate Margins of the Fram Strait (Svalbard and eastern North Greenland), Indicated by Low-temperature Thermochronology", submitted to the journal Geochemistry, Geophysics, Geosystems. The data include apatite (U-Th-Sm)/He analyses (table S2) and apatite fission track analyses (dataset S1). We used the thermochronology data to derive time-temperature histories. In the document "Supporting Information", we provide the analytical protocols (Text S1-3, S5), data visualization and assessment for influences and relationships (Figures S2, S3, S4), modelling strategy, parameters and results (Text S4, Figure S5, Table S3), and thin section analyses of the host rock and associated quartz veins (Figures S6-9, Table S4-5). It also contains a summary of the analysed samples, their sampling locations and the resulting AFT and AHe ages (Table S1).

The simulation data generated are from two sources: validation for the breakup model is accomplished by solving a system of population balance equations (the “ODE model.†). A large-eddy simulation (LES) is used to model oil droplets transported by a turbulent jet subjected to a uniform cross-flow. The breakup model is compared to the experimental results of Eastwood et al (2004). Data used to create the figures in the associated paper are included in this dataset. In addition to a series of Readme files, a dataset description document describe the structure of the dataset and the variable names and units. This dataset supports the publication: Aiyer, A. K., Yang, D., Chamecki, M., & Meneveau, C. (2019). A population balance model for large eddy simulation of polydisperse droplet evolution. Journal of Fluid Mechanics, 878, 700–739. doi:10.1017/jfm.2019.649

This 2D multi-channel seismic data set was acquired during SONNE cruise SO241 offshore Mexico in the Guaymas Basin in June 2015. MCS data were collected using a Geometrics GeoEel streamer of variable active lengths, such as 150, 162, 175, and 187 m with 96, 104, 112, and 120 channels, respectively. The hydrophone group spacing was 1.56 m. The seismic source signal was generated by two generator-injector (GI) air guns, each with a volume of 210 cubic inches or 3.44 l (1.72 l generator and 1.72 l injector). The air guns were operated in harmonic mode at a tow depth of 2 m. The shot interval was 7 s, resulting in a mean shot point distance of 12 m. The recording time was 4 s, and the sampling rate was 1 ms. Navigation is based on ship GPS and lay backs. Locations are given in UTM zone 12N. Seismic data processing was funded by VBPR AS and carried out with RadExPro. It included common mid-point (CMP) binning with a CMP bin spacing of 3.125 m; band pass filtering using an Ormsby filter with corner frequencies of 20, 45, 250, and 400 Hz; normal move-out correction (NMO); and true amplitude recovery. The NMO-corrected gathers were stacked, and subsequently, a post-stack Stolt migration with 1500 m/s velocity was carried out. Detailed information on the data acquisition can be found in the SO241 cruise report (https://doi.org/10.3289/CR_S241).

Ice breakup dates of Chequamegon Bay, Lake Superior from 1911 to 2021 were compiled by Lori Evrard (USGS, GLSC, Lake Superior Biological Station, Ashland, WI). Ice breakup date is the day in spring when winter ice cover substantially leaves a water body. Local residents deem "ice breakup" as when the ice moves northeast of a line straight across Chequamegon Bay out from Ellis Avenue (State highway 13). Another way ice breakup was determined has been if you could drive a boat from the outlet of Fish Creek to Houghton Point. The ice may move back and forth over that line but the ice is breaking up, moving and melting from that date on. Ellis Avenue ends on a bluff (46.5925 degrees North, 90.8827 degrees West) that provides a clear view of Chequamegon Bay from Fish Creek to Houghton Point. Mrs. C. J. Hoskings recorded the dates from 1911 to 1980. Mr. LeRoy C. Margenau recorded the dates from 1981 to 1991. The Ashland Marina recorded the dates from 1992-1999 and 2001. Lori Evrard (USGS) recorded dates after 1999 except 2001. USGS converted each date to a consecutive day of the year value. The date of ice breakup will be updated annually to append that year's date.

Statistics illustrates consumption, production, prices, and trade of Vessels and other floating structures; for breaking up in Burkina Faso from 2007 to 2024.