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関連する概念動画

Radiation: Applications01:17

Radiation: Applications

1.1K
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...
1.1K
Global Climate Change01:50

Global Climate Change

24.3K
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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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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Mechanisms of Heat Transfer II01:20

Mechanisms of Heat Transfer II

3.2K
In convection, thermal energy is carried by the large-scale flow of matter. Ocean currents and large-scale atmospheric circulation, which result from the buoyancy of warm air and water, transfer hot air from the tropics toward the poles and cold air from the poles toward the tropics. The Earth’s rotation interacts with those flows, causing the observed eastward flow of air in the temperate zones. Convection dominates heat transfer by air, and the amount of available space for the airflow...
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What is Weather?01:07

What is Weather?

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Overview
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Thermometers and Temperature Scales01:22

Thermometers and Temperature Scales

5.3K
Any physical property that depends consistently and reproducibly on temperature can be used as the basis of a thermometer. For example, volume increases with temperature for most substances. This property is the basis for the common alcohol thermometer and the original mercury thermometers. Other properties used to measure temperature include electrical resistance, color, and the emission of infrared radiation.
As many physical properties depend on temperature, the variety of thermometers is...
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Updated: Jun 12, 2025

Simulating Temperature in a Soil Incubation Experiment
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Simulating Temperature in a Soil Incubation Experiment

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熱い地球と冷たい地球

Benjamin J W Mills1

  • 1School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK.

Science (New York, N.Y.)
|September 19, 2024
PubMed
まとめ
この要約は機械生成です。

古代 の 地球

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A Gusseted Thermogradient Table to Control Soil Temperatures for Evaluating Plant Growth and Monitoring Soil Processes
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関連する実験動画

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Thermocapillary Convection Space Experiment on the SJ-10 Recoverable Satellite
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科学分野:

  • 古代気候学
  • 地球システム科学

背景:

  • 地球の過去の気候を理解することは 将来の気候変動を予測するのに不可欠です
  • 古代の気温を再構築することで 長期の気候の動態に関する洞察が得られます

研究 の 目的:

  • 古代の地球の気温記録を 復元するために
  • グローバルな気候規制システムのメカニズムを特定し理解する.

主な方法:

  • 古気候のプロキシ (例えば,氷核,堆積層) の分析.
  • 過去の状況とシステムのフィードバックをシミュレートする気候モデリング.

主要な成果:

  • 古代の地球温度の詳細な再構築
  • 地質学的スケールで 地球の温度を安定させた 自律的な気候システムの証拠です

結論:

  • 地球には固有の気候制御システムがあります
  • このシステムは 地球の歴史を通して 居住可能な状態を維持する上で 重要な役割を果たしました