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Global Climate Change01:50

Global Climate Change

Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
What is Weather?01:07

What is Weather?

Overview
What is Climate?01:16

What is Climate?

Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
Precipitation and Co-precipitation01:17

Precipitation and Co-precipitation

Precipitation and coprecipitation methods can be used to separate a mixture of ions in a solution. In qualitative inorganic analysis, ions that form sparingly soluble precipitates with the same reagent are separated based on the differences in solubility products. For example, consider the separation of Cu(II) and Fe(II) ions by precipitation as insoluble sulfides. First, copper(II) sulfide is precipitated by the addition of acidic H2S, where the dissociation of H2S is suppressed. Adding H2S...
Precipitation Processes01:12

Precipitation Processes

The experimental conditions in a gravimetric analysis should be optimized to maximize the particle size and purity of the obtained precipitate. Ideally, the concentration of the precipitating reagent should be low with effective stirring to maintain low relative supersaturation for the growth of large crystals. In homogeneous precipitation, the precipitant is slowly generated by a chemical reaction in the solution to avoid local reagent excesses. For example, urea decomposes gradually to...
Microbes and Climate Change01:27

Microbes and Climate Change

Microorganisms are pivotal agents in Earth's biogeochemical cycles, significantly influencing climate dynamics through their metabolic activities. These microbes modulate the levels of key greenhouse gases by both contributing to and helping mitigate climate change.Microbial Contributions to Greenhouse Gas EmissionsRising global temperatures accelerate microbial metabolism, which, in turn, speeds up the decomposition of organic matter. This process releases carbon dioxide (CO₂) through...

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Updated: Jul 14, 2026

Simulating Impacts of Ice Storms on Forest Ecosystems
06:27

Simulating Impacts of Ice Storms on Forest Ecosystems

Published on: June 30, 2020

地球温暖化がもたらす雨量はどのくらい増えるのでしょうか?

Frank J Wentz1, Lucrezia Ricciardulli, Kyle Hilburn

  • 1Remote Sensing Systems, 438 First Street, Santa Rosa, CA 95401, USA. frank.wentz@remss.com

Science (New York, N.Y.)
|June 2, 2007
PubMed
まとめ

地球温暖化により大気中の水蒸気はケルビンあたり7%増加する. しかし,衛星データによると,降水量は同じペースで増加しており,気候モデルの予測に反して,増加が遅くなっている.

科学分野:

  • 大気科学 大気科学
  • 気候科学 気候科学
  • リモートセンシングによる遠隔感知

背景:

  • 気候モデルでは,温暖化の1ケルビンあたり,大気中の水の7%の増加を予測しています.
  • 現在の気候モデルでは,世界の降水量がよりゆっくりと増加すると予測されています (ケルビンあたり1-3%).

研究 の 目的:

  • 気候モデルの降水予測と衛星観測を比較する.
  • 大気中の水と降水量の変化の間の観察された関係を調査する.

主な方法:

  • 大気中の水と降水に関する衛星観測の分析.
  • 観測された傾向と気候モデルの出力との比較.

主要な成果:

  • 衛星データは,温暖化のケルビンあたり約7%の降雨の増加を示しています.
  • 観測された降水量の増加は,大気中の水の増加率と一致します.
  • これは,減量の降雨反応に関する気候モデルの予測と矛盾している.

結論:

  • 最近の衛星観測は,温暖化への降雨反応の気候モデル予測に異議を唱えている.
  • この発見は,降水量が以前モデル化されていたよりも地球温暖化に敏感である可能性があることを示唆している.

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Last Updated: Jul 14, 2026

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Using Generative Art to Convey Past and Future Climate Transitions
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Using Generative Art to Convey Past and Future Climate Transitions

Published on: March 31, 2023