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関連する概念動画

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.
Isothermal Processes01:21

Isothermal Processes

A thermodynamic process that occurs at constant temperature is called an isothermal process. Heat slowly flows into the system or out of the system to maintain thermal equilibrium. Processes involving phase changes like water evaporation into steam or freezing water into ice at a constant temperature are examples of Isothermal Processes.
An ideal gas can also undergo isothermal expansion or compression.
For example, consider 1 mole of an ideal gas inside an isolated cylinder at initial volume V...
Isochoric and Isobaric Processes01:21

Isochoric and Isobaric Processes

A thermodynamic process that occurs at constant volume is called an isochoric process. According to the first law of thermodynamics, heat supplied or removed from the system is partially utilized to perform work and change the internal energy of the system. However, in an isochoric process, the volume remains constant. Hence, the work done by the system is zero. Therefore, the exchange of heat changes the internal energy of the system only. 
Suppose 1000 g of water is heated from 40 degrees...
Damped Oscillations01:07

Damped Oscillations

In the real world, oscillations seldom follow true simple harmonic motion. A system that continues its motion indefinitely without losing its amplitude is termed undamped. However, friction of some sort usually dampens the motion, so it fades away or needs more force to continue. For example, a guitar string stops oscillating a few seconds after being plucked. Similarly, one must continually push a swing to keep a child swinging on a playground.
Although friction and other non-conservative...
Speciation Rates01:07

Speciation Rates

Speciation can proceed at markedly different rates, and evolutionary biologists commonly describe these differences through the models of gradualism and punctuated equilibrium. Both patterns explain how new species arise, but they differ in the tempo and continuity of evolutionary change. In both cases, evolutionary change arises from heritable variation within populations, with natural selection often shaping traits that improve survival and reproduction under specific environmental conditions.
Precipitation Gravimetry01:03

Precipitation Gravimetry

Precipitation gravimetry is based on converting an analyte into a sparingly soluble precipitate, which is separated by filtration and weighed. An ideal precipitate should be pure, insoluble, of known composition, and easily filtered from the reaction mixture.
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...

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関連する実験動画

Updated: Jun 17, 2026

Evolution of Staircase Structures in Diffusive Convection
07:28

Evolution of Staircase Structures in Diffusive Convection

Published on: September 5, 2018

同期的な脱氷転覆と水質源の変化

Natalie L Roberts1, Alexander M Piotrowski, Jerry F McManus

  • 1Godwin Laboratory for Palaeoclimate Research, Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, UK. nr297@cam.ac.uk

Science (New York, N.Y.)
|January 2, 2010
PubMed
まとめ

最後の脱氷期における海洋循環の変化は同期的であり,深い水の源と転覆率に影響を与えた. ハインリッヒ事件1のようなミレニアム規模のイベントは,全海洋の気候変化とは異なる浅い転覆のみに影響しました.

科学分野:

  • パレオセアノグラフィー
  • 気候科学 気候科学
  • 地質化学 地質化学

背景:

  • 海洋循環のダイナミクスを理解することは,過去の気候変動の解読の鍵です.
  • 最後の脱氷は,急激な気候変動のメカニズムへの重要な窓を提供します.
  • 深海の変化の再構築は,世界の気候モデルに情報を与えます.

研究 の 目的:

  • 最後の脱氷期における北大西洋の深い西部の地下水源の変化を再建する.
  • 深水の質量源のシフトと海洋の転覆率を比較するために.
  • ミレニアム規模の気候変動の影響を,脱氷期の移行から区別する.

主な方法:

  • 鉄・マンガン酸化物コーティングのネオジムイソトープ測定.
  • ベルミューダ・ライズからのプランクトンフォラミニフェラの分析.
  • 海洋の転覆強度に関する既存のプロキシと比較.

主要な成果:

  • 深い水の質量源と転覆率は,最後の脱氷期の移行期に迅速かつ同期的に変化した.
  • ハインリッヒイベント1からの淡水乱れは,浅い海の転覆にのみ影響した可能性がある.
  • 異なる気候フォースリングに対する深い対浅い海洋の転覆の明確な反応が観察されました.

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

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
10:28

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information

Published on: June 13, 2020

関連する実験動画

Last Updated: Jun 17, 2026

Evolution of Staircase Structures in Diffusive Convection
07:28

Evolution of Staircase Structures in Diffusive Convection

Published on: September 5, 2018

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

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
10:28

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information

Published on: June 13, 2020

結論:

  • 脱氷期における海洋循環の変化は,迅速かつ同期的であり,水柱全体に影響を与えた.
  • ミレニアムスケールの気候現象は,主要な脱氷現象と比較して,海洋循環により局所的な影響を及ぼします.
  • この研究は,地球の気候変動の移行を調節する海洋の役割に関する私たちの理解を洗練します.