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- https://bio.libretexts.org/Sandboxes/tholmberg_at_nwcc.edu/Introduction_to_Environmental_Science/6%3A_Climate_Change/6.2%3A_Anthropogenic_Climate_ChangeQuantitative evidence supports the relationship between atmospheric concentrations of carbon dioxide and temperature: as carbon dioxide rises global temperature rises. Qualitative evidence of climate ...Quantitative evidence supports the relationship between atmospheric concentrations of carbon dioxide and temperature: as carbon dioxide rises global temperature rises. Qualitative evidence of climate change exists as well. The current increase in atmospheric carbon dioxide has happened very quickly—in a matter of hundreds of years rather than thousands of years. As more and more of the world's population adopts a resource-intensive lifestyle the climate problem becomes worse.
- https://bio.libretexts.org/Workbench/General_Ecology_Ecology/Chapter_2%3A_The_Physical_Environment/2.5%3A_Earth's_Energy_BalanceEarth’s temperature depends on the balance between energy entering and leaving the planet. When incoming energy from the sun is absorbed, Earth warms. When energy is released from Earth into space, th...Earth’s temperature depends on the balance between energy entering and leaving the planet. When incoming energy from the sun is absorbed, Earth warms. When energy is released from Earth into space, the planet cools. Many factors, both natural and human, can cause changes in Earth’s energy balance, including changes in greenhouse gasses; variations in the sun’s energy reaching Earth; and changes in the reflectivity of Earth’s atmosphere and surface.
- https://bio.libretexts.org/Workbench/General_Ecology_Ecology/Chapter_5%3A_Terrestrial_and_Aquatic_Communities/5.1%3A_Earth's_Biomes/5.1.4%3A_Climate_and_the_Effects_of_Global_Climate_ChangeAll biomes are universally affected by global conditions, such as climate, that ultimately shape each biome’s environment. Scientists who study climate have noted a series of marked changes that have ...All biomes are universally affected by global conditions, such as climate, that ultimately shape each biome’s environment. Scientists who study climate have noted a series of marked changes that have gradually become increasingly evident during the last sixty years. Global climate change is the term used to describe altered global weather patterns, including a worldwide increase in temperature, due largely to rising levels of atmospheric carbon dioxide.
- https://bio.libretexts.org/Bookshelves/Introductory_and_General_Biology/Biology_(Kimball)/02%3A_The_Molecules_of_Life/2.08%3A_EnantiomersThis page explains the tetrahedral arrangement of carbon atoms forming four covalent bonds, exemplified by methane. It discusses how the presence of different groups around carbon can lead to enantiom...This page explains the tetrahedral arrangement of carbon atoms forming four covalent bonds, exemplified by methane. It discusses how the presence of different groups around carbon can lead to enantiomers, using alanine as an example of L- and D- formations, emphasizing the predominance of L amino acids in protein synthesis. Chirality's importance is highlighted, noting that a protein's functionality depends on its shape.
- https://bio.libretexts.org/Courses/University_of_Vermont/UVM_Environmental_Science/07%3A_Atmosphere_and_Air_Pollution/7.02%3A_Earth's_Energy_BalanceEarth’s temperature depends on the balance between energy entering and leaving the planet. When incoming energy from the sun is absorbed, Earth warms. When energy is released from Earth into space, th...Earth’s temperature depends on the balance between energy entering and leaving the planet. When incoming energy from the sun is absorbed, Earth warms. When energy is released from Earth into space, the planet cools. Many factors, both natural and human, can cause changes in Earth’s energy balance, including changes in greenhouse gasses; variations in the sun’s energy reaching Earth; and changes in the reflectivity of Earth’s atmosphere and surface.
- https://bio.libretexts.org/Courses/Monterey_Peninsula_College/Raskoff_Environmental_Science/09%3A_Climate/9.07%3A_Climate_ChangeEarth’s temperature depends on the balance between energy entering and leaving the planet. When incoming energy from the sun is absorbed, Earth warms. When the sun’s energy is reflected back into spac...Earth’s temperature depends on the balance between energy entering and leaving the planet. When incoming energy from the sun is absorbed, Earth warms. When the sun’s energy is reflected back into space, Earth avoids warming. When energy is released from Earth into space, the planet cools. Many factors, both natural and human, can cause changes in Earth’s energy balance.
- https://bio.libretexts.org/Courses/Monterey_Peninsula_College/Raskoff_Environmental_Science/09%3A_ClimateThis chapter examines Earth's climate and atmospheric evolution, starting with cyanobacteria's oxygen production 3.5 billion years ago. It covers the Quaternary period and human evolution, discusses f...This chapter examines Earth's climate and atmospheric evolution, starting with cyanobacteria's oxygen production 3.5 billion years ago. It covers the Quaternary period and human evolution, discusses factors affecting global climate change and observed temperature rises, and emphasizes the need for scientific models rooted in thorough data to understand these changes.
- https://bio.libretexts.org/Workbench/General_Ecology_Ecology/Chapter_2%3A_The_Physical_Environment/2.7%3A_What_Makes_the_Climate_ChangeFor example, the opening of the Drake Passage — due to plate-tectonic separation of South America from Antarctica — led to the development of the Antarctic Circumpolar Current, which isolated Antarcti...For example, the opening of the Drake Passage — due to plate-tectonic separation of South America from Antarctica — led to the development of the Antarctic Circumpolar Current, which isolated Antarctica from the warmer water in the rest of the ocean and thus contributed to Antarctic glaciation starting at around 35 Ma.
- https://bio.libretexts.org/Bookshelves/Biochemistry/Fundamentals_of_Biochemistry_(Jakubowski_and_Flatt)/Unit_IV_-_Special_Topics/32%3A_Biochemistry_and_Climate_Change/32.01A%3A__The_Basics_of_Climate_ChangeIn December 2023, a refinement of CO 2 , temperature, and sea level rise data since the demise of the dinosaurs 65 million years ago was published. (The geological interval from 66 million years ago t...In December 2023, a refinement of CO 2 , temperature, and sea level rise data since the demise of the dinosaurs 65 million years ago was published. (The geological interval from 66 million years ago to now is called the Cenozoic Era and consists of 3 periods: the Paleogene until 23 MYA, the Neogene until 2.6 MYA, and the Quaternary.) A group, the Cenozoic Carbon Dioxide Proxy Integration Project (CenCO2PIP) Consortium, reviewed and reevaluated all "proxy" measurements used to determine past cli…
- https://bio.libretexts.org/Bookshelves/Introductory_and_General_Biology/Biology_(Kimball)/02%3A_The_Molecules_of_Life/2.02%3A_HydrocarbonsThis page discusses hydrocarbons, organic compounds made of carbon and hydrogen, categorized into aliphatic (linear chains) and aromatic (ring structures). Aliphatic hydrocarbons include saturated com...This page discusses hydrocarbons, organic compounds made of carbon and hydrogen, categorized into aliphatic (linear chains) and aromatic (ring structures). Aliphatic hydrocarbons include saturated compounds like methane and unsaturated types like ethylene. Aromatic hydrocarbons are based on benzene rings and occur in biological molecules, including amino acids, cholesterol, and hormones. Beta-carotene is highlighted as a hydrocarbon containing both aliphatic and aromatic components.
- https://bio.libretexts.org/Courses/University_of_Vermont/UVM_Environmental_Science/07%3A_Atmosphere_and_Air_Pollution/7.01%3A_The_AtmosphereThe atmosphere, the gaseous layer that surrounds the earth, formed over four billion years ago and is held in place by the attractive forces of gravity. This section is a brief introduction to the lay...The atmosphere, the gaseous layer that surrounds the earth, formed over four billion years ago and is held in place by the attractive forces of gravity. This section is a brief introduction to the layers of the atmosphere and the differences between climate and weather.
