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What is Weather?01:07

What is Weather?

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Overview
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What is Climate?01:16

What is Climate?

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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.
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Global Climate Change01:50

Global Climate Change

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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.
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Threats to Biodiversity01:50

Threats to Biodiversity

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There have been five major extinction events throughout geological history, resulting in the elimination of biodiversity, followed by a rebound of species that adapted to the new conditions. In the current geological epoch, the Holocene, there is a sixth extinction event in progress. This mass extinction has been attributed to human activities and is thus provisionally called the Anthropocene. In 2019 the human population reached 7.7 billion people and is projected to comprise 10 billion by...
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Radiation: Applications01:17

Radiation: Applications

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The average temperature of Earth is the subject of much current discussion. Earth is in radiative contact with both the Sun and dark space; it receives almost all its energy from the radiation of the Sun and reflects some of it into outer space. Dark space is very cold, about 3 K, so Earth radiates energy into it. For instance, heat transfer occurs from soil and grasses, the rate of which can be so rapid that frost can occur on clear summer evenings, even in warm latitudes.
The average...
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Microbes and Climate Change01:27

Microbes and Climate Change

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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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Causes of irregularities in trends of global mean surface temperature since the late 19th century.

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Design and Construction of an Urban Runoff Research Facility
13:48

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Published on: August 8, 2014

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気候:大規模な温暖化は都市では起こらない.

David E Parker1

  • 1Hadley Centre, Meteorological Office, Exeter EX1 3PB, UK. david.parker@metoffice.com

Nature
|November 19, 2004
PubMed
まとめ

地球温暖化傾向は都市開発によるものではない. この研究は,風の強い夜と穏やかな夜に陸地の気温が等しく上昇したことを示し,温暖化の主要な要因として都市熱島効果を否定しています.

科学分野:

  • 気候学 気候学
  • 大気科学 大気科学
  • 都市気象学 都市気象学

背景:

  • 都市温暖化の影響が,大規模な地表気温動向に及ぼす影響について,継続的な議論が行われています.
  • 都市熱島 (UHIs) は,主に夜間の気温に影響し,風の強い条件下では減少することが知られている.

研究 の 目的:

  • 都市温暖化が地球上の地表気温の動向に影響を与えているかどうかを調査する.
  • 観測された気候温暖化における都市開発の役割を決定する.

主な方法:

  • 全世界の陸地表面空気の気温データを分析し,風の強い夜間と静かな夜間を区別する.
  • 都市熱島の影響を隔離するために,異なる風速の下での気温動向の比較.

主要な成果:

  • 地球全体の陸地温度は,風が吹く夜と静かな夜の両方で,比較的に上昇しています.
  • 風の強い夜における温暖化の速度は,静かな夜における温暖化の速さと同様のもので,大規模なトレンドに関するUHI仮説に異議を唱える.

結論:

  • 観測された地球温暖化傾向は,都市開発の結果である可能性は低い.
  • 都市熱島効果は,大規模な気温上昇を誘発する主要な要因ではないようです.

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