About this dataset

Context

The dataset tabulates the Non-Hispanic population of White Earth by race. It includes the distribution of the Non-Hispanic population of White Earth across various race categories as identified by the Census Bureau. The dataset can be utilized to understand the Non-Hispanic population distribution of White Earth across relevant racial categories.

Key observations

With a zero Hispanic population, White Earth is 100% Non-Hispanic. Among the Non-Hispanic population, the largest racial group is White alone with a population of 76 (100% of the total Non-Hispanic population).

Content

When available, the data consists of estimates from the U.S. Census Bureau American Community Survey (ACS) 2018-2022 5-Year Estimates.

Racial categories include:

• White
• Black or African American
• American Indian and Alaska Native
• Asian
• Native Hawaiian and Other Pacific Islander
• Some other race
• Two or more races (multiracial)

Variables / Data Columns

• Race: This column displays the racial categories (for Non-Hispanic) for the White Earth
• Population: The population of the racial category (for Non-Hispanic) in the White Earth is shown in this column.
• % of Total Population: This column displays the percentage distribution of each race as a proportion of White Earth total Non-Hispanic population. Please note that the sum of all percentages may not equal one due to rounding of values.

Good to know

Margin of Error

Data in the dataset are based on the estimates and are subject to sampling variability and thus a margin of error. Neilsberg Research recommends using caution when presening these estimates in your research.

Custom data

If you do need custom data for any of your research project, report or presentation, you can contact our research staff at research@neilsberg.com for a feasibility of a custom tabulation on a fee-for-service basis.

Inspiration

Neilsberg Research Team curates, analyze and publishes demographics and economic data from a variety of public and proprietary sources, each of which often includes multiple surveys and programs. The large majority of Neilsberg Research aggregated datasets and insights is made available for free download at https://www.neilsberg.com/research/.

Recommended for further research

This dataset is a part of the main dataset for White Earth Population by Race & Ethnicity. You can refer the same here

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Introduction:

Carbon dioxide (CO₂) is the most abundant greenhouse gas emitted by human activities. The burning of fossil fuels, such as coal, oil, and natural gas, is the primary source of CO₂ emissions. Other human activities, such as deforestation and industrial processes, also contribute to CO₂ emissions.

CO₂ emissions are a major driver of climate change. Climate change is the long-term alteration of temperature and typical weather patterns in a place. Climate change could refer to a particular location or the planet as a whole. Climate change may cause weather patterns to be less predictable. A region might experience lower or higher-than-average temperatures. Climate change may cause more frequent and severe weather events, such as storms, floods, and droughts.

Hurricane Beryl: Caribbean leader calls out rich countries for climate failures as ‘horrendous’ storm makes landfall. link

The effects of climate change are already being felt around the world, and they are expected to become more severe in the future. These effects include rising sea levels, more extreme weather events, changes in precipitation patterns, and loss of biodiversity.

Carl Sagan testified before Congress in 1985 on climate change.link

Unveiling the Composition of Air - A Glimpse into Earth's Breath: - Introduction: - Air, an essential and seemingly ubiquitous part of our daily lives, has a composition that remained a mystery for centuries. Only through groundbreaking discoveries and experiments did scientists unravel the complex tapestry of gases that make up Earth's atmosphere. - The Elemental Journey: - Ancient Greeks, over 2,500 years ago, identified air, along with earth, fire, and water, as fundamental elements of creation. However, it took until the late 18th century for this perspective to be challenged by the daring English chemist Joseph Priestley. His experiments shattered the belief that air was an elementary substance, revealing it as a composite mixture of gases. - Priestley's Revelation: - In 1774, Priestley's experiments led to the identification of "dephlogisticated air," later named oxygen by Antoine Lavoisier. This groundbreaking discovery marked the end of a 23-century-old notion that air was indestructible and unalterable, opening the door to a more sophisticated understanding of the gases enveloping our planet. - The Mid-18th Century and Elemental Evolution: - During the mid-18th century, the concept of elements was evolving, with researchers grappling to understand the nature of air and its role in chemical processes. The era saw a surge of interest in gases, driven by the transformative impact of the steam engine on civilisation. - British Chemists and Gas Exploration: - British chemists, including Joseph Black and Henry Cavendish, played a pivotal role in exploring gases. Black identified "fixed air" (now carbon dioxide) in 1754, and Cavendish produced hydrogen in 1766. - Daniel Rutherford's 1772 experiments led to the discovery of nitrogen, as he burned material in a bell jar, leaving behind a gas termed "noxious air." - Conclusion: - The composition of air, once thought to be a simple and unalterable substance, has been unveiled through the efforts of pioneering scientists. Priestley's revelation of oxygen, along with contributions from fellow chemists, has reshaped our understanding of the gases that constitute Earth's atmosphere. In this delicate balance of elements, air reveals itself as a dynamic and essential force, sustaining life on our planet.

The composition of air.

The air we breathe is primarily composed of a mixture of gases. The approximate composition of dry air, excluding water vapour, is as follows:

1. Nitrogen (N₂) - Approximately 78%
2. Oxygen (O₂) - Approximately 21%
3. Argon (Ar) - Approximately 0.93%
4. Carbon Dioxide (CO₂) - Approximately 0.04%
5. Neon (Ne) - Approximately 0.0018%
6. Helium (He) - Approximately 0.0005%
7. Methane (CH₄) - Approximately 0.0002%
8. Krypton (Kr) - Approximately 0.0001%
9. Hydrogen (H₂) - Approximately 0.00005%
10. Xenon (Xe) - Approximately 0.000009%

Additionally, trace amounts of other gases, such as ozone (O₃), nitrogen oxides (NOx), and sulphur dioxide (SO₂), are present in the atmosphere.

It's important to note that these percentages can vary slightly based on factors such as location, altitude, and environmental conditions. Water vapour is also a variable component of the atmosphere, with its concentration ranging from near zero to about 4% in humid conditions.

Greenhouse Effect:

The study of the greenhouse effect and global warming has a fascinating history, and it's amazing to see how early scientists like Arrhenius and Callendar laid the ground...

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