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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

全球变暖会带来多少更多的雨?

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
概括

全球变暖使大气中的水蒸气每克尔文增加7%. 然而,卫星数据显示降水量以同样的速度上升,这与气候模型预测的较慢增长相矛盾.

科学领域:

  • 大气科学 大气科学
  • 气候科学是气候科学.
  • 遥感是一种远程传感.

背景情况:

  • 气候模型预测大气中的水量每克尔文升温增加7%.
  • 目前的气候模型预测全球降水增速将较慢 (每凯尔文为1-3%).

研究的目的:

  • 将气候模型降水预测与卫星观测进行比较.
  • 为了研究大气水和降水变化之间观察到的关系.

主要方法:

  • 对大气水和降水的卫星观测结果的分析.
  • 观察到的趋势与气候模型输出的比较.

主要成果:

  • 卫星数据显示,降水量每克尔文升温大约增加7%.
  • 观测到的降水增加与大气总水增加的速度相匹配.
  • 这与气候模型预测的降水反应减弱的情况相矛盾.

结论:

  • 最近的卫星观测挑战了气候模型对降雨对变暖反应的预测.
  • 这些发现表明,降水对全球变暖的敏感度可能比以前建模的更高.

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Last Updated: Jul 14, 2026

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