Jove
Visualize
お問い合わせ
JoVE
x logofacebook logolinkedin logoyoutube logo
JoVEについて
概要リーダーシップブログJoVEヘルプセンター
著者向け
出版プロセス編集委員会範囲と方針査読よくある質問投稿
図書館員向け
推薦の声購読アクセスリソース図書館諮問委員会よくある質問
研究
JoVE JournalMethods CollectionsJoVE Encyclopedia of Experimentsアーカイブ
教育
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab Manual教員リソースセンター教員サイト
利用規約
プライバシーポリシー
ポリシー

関連する概念動画

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.
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.
Responses to Heat and Cold Stress02:45

Responses to Heat and Cold Stress

Every organism has an optimum temperature range within which healthy growth and physiological functioning can occur. At the ends of this range, there will be a minimum and maximum temperature that interrupt biological processes.
Radiation: Applications01:17

Radiation: Applications

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...
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...

こちらも読む

関連記事

共著者、ジャーナル、引用グラフによってこの研究に関連する記事。

並び替え
Same author

Response to Comment on "Atlantic and Pacific multidecadal oscillations and Northern Hemisphere temperatures".

Science (New York, N.Y.)·2015
Same author

Implications of temperature variation for malaria parasite development across Africa.

Scientific reports·2013
Same author

Solar forcing of regional climate change during the Maunder Minimum.

Science (New York, N.Y.)·2001
Same author

The scope of Medieval warming.

Science (New York, N.Y.)·2001
Same author

Comparison of phenytoin with noncompetitive N-methyl-D-aspartate antagonists in a model of focal brain ischemia in rat.

Stroke·1990
Same author

Air embolism associated with veno-venous bypass during orthotopic liver transplantation.

Anesthesiology·1987

関連する実験動画

Updated: Jul 9, 2026

Simulating Temperature in a Soil Incubation Experiment
08:39

Simulating Temperature in a Soil Incubation Experiment

Published on: October 28, 2022

気候変動:新しいミレニアムの教訓

M E Mann

    Science (New York, N.Y.)
    |August 31, 2007
    PubMed
    まとめ

    単純な気候モデルのシミュレーションは,人為的な温室効果ガスの増加が地球温暖化を引き起こしているという説得力のある証拠を提供します. この研究は,過去の気候変動を明らかにし,現在の温暖化傾向についての理解を強化します.

    科学分野:

    • 気候科学 気候科学
    • 古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは
    • 大気モデリング

    背景:

    • 過去の気候変化を理解することは,現在の気候変化の評価に不可欠です.
    • 複雑な海洋大気モデルには,気候の動態をシミュレートする際の限界があります.
    • 温暖化に対する人間の影響に関する以前の研究は,しばしば複雑なモデルに依存していた.

    研究 の 目的:

    • 簡素化されたモデルを使用して,過去千年の気候変化をシミュレートする.
    • 地球温暖化に対する人間の影響を評価する.
    • 人為的な地球温暖化に関する説得力のあるケースを提示するために.

    主な方法:

    • 主要な自然および人為的な気候強制を組み込んだ単純な気候モデルを使用しました.
    • 過去千年にわたるシミュレーションされた気候の変化.
    • モデルの出力を観察データと比較した.

    主要な成果:

    • このシンプルなモデルは,過去1千年における気候変化をうまくシミュレートした.

    さらに関連する動画

    Using Generative Art to Convey Past and Future Climate Transitions
    06:10

    Using Generative Art to Convey Past and Future Climate Transitions

    Published on: March 31, 2023

    Façade-Level Monitoring of CO2 Variability under Urban Heat Island Conditions using Low-Cost Sensor Data Loggers
    07:12

    Façade-Level Monitoring of CO2 Variability under Urban Heat Island Conditions using Low-Cost Sensor Data Loggers

    Published on: December 12, 2025

    関連する実験動画

    Last Updated: Jul 9, 2026

    Simulating Temperature in a Soil Incubation Experiment
    08:39

    Simulating Temperature in a Soil Incubation Experiment

    Published on: October 28, 2022

    Using Generative Art to Convey Past and Future Climate Transitions
    06:10

    Using Generative Art to Convey Past and Future Climate Transitions

    Published on: March 31, 2023

    Façade-Level Monitoring of CO2 Variability under Urban Heat Island Conditions using Low-Cost Sensor Data Loggers
    07:12

    Façade-Level Monitoring of CO2 Variability under Urban Heat Island Conditions using Low-Cost Sensor Data Loggers

    Published on: December 12, 2025

  • モデル結果は観察データと一致し,研究の主張を支持します.
  • クロウリーの研究は,人類による地球温暖化の強い根拠を示しています.
  • 結論:

    • 人為的な温室効果ガスの増加は,最近の地球温暖化の主要な原動力である.
    • 簡素化された気候モデルは,過去の気候変動を効果的にシミュレートすることができます.
    • この研究は,地球温暖化に人類が及ぼす影響の理解を深めるものです.