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関連する概念動画

Global Climate Change01:50

Global Climate Change

24.6K
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.
24.6K
Thermal Sigmatropic Reactions: Overview01:16

Thermal Sigmatropic Reactions: Overview

2.1K
Sigmatropic rearrangements are a class of pericyclic reactions in which a σ bond migrates from one part of a π system to another. These are intramolecular rearrangements where the total number of σ and π bonds remain unchanged.
Sigmatropic shifts are classified based on an order term [i, j ], where i and j indicate the number of atoms across which each end of the σ bond migrates. Below are examples of a [3,3] sigmatropic shift in...
2.1K
Phase Transitions: Melting and Freezing02:39

Phase Transitions: Melting and Freezing

12.5K
Heating a crystalline solid increases the average energy of its atoms, molecules, or ions, and the solid gets hotter. At some point, the added energy becomes large enough to partially overcome the forces holding the molecules or ions of the solid in their fixed positions, and the solid begins the process of transitioning to the liquid state or melting. At this point, the temperature of the solid stops rising, despite the continual input of heat, and it remains constant until all of the solid is...
12.5K
Isochoric and Isobaric Processes01:21

Isochoric and Isobaric Processes

3.5K
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...
3.5K
Phase Transitions: Sublimation and Deposition02:33

Phase Transitions: Sublimation and Deposition

17.3K
Some solids can transition directly into the gaseous state, bypassing the liquid state, via a process known as sublimation. At room temperature and standard pressure, a piece of dry ice (solid CO2) sublimes, appearing to gradually disappear without ever forming any liquid. Snow and ice sublimate at temperatures below the melting point of water, a slow process that may be accelerated by winds and the reduced atmospheric pressures at high altitudes. When solid iodine is warmed, the solid sublimes...
17.3K
Isothermal Processes01:21

Isothermal Processes

3.8K
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...
3.8K

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関連する実験動画

Updated: Aug 6, 2025

Using Generative Art to Convey Past and Future Climate Transitions
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Using Generative Art to Convey Past and Future Climate Transitions

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北極海の海氷の厚さの変化

Hiroshi Sumata1, Laura de Steur2, Dmitry V Divine2

  • 1Norwegian Polar Institute, Fram Centre, Tromsø, Norway. hiroshi.sumata@npolar.no.

Nature
|March 16, 2023
PubMed
まとめ

2007年に北極の海氷は 厚い氷から薄い氷へと変化し 海氷の保存期間が短縮されました 気候変化が北極の海氷に及ぼす 長期的な影響は 海洋氷の重要な過程を 強調しています

科学分野:

  • 気候科学
  • 海洋学
  • クリオスフィアの研究

背景:

  • 気候変動の影響は 徐々に起こりますが 気候システムは 急激に変化します
  • 北極の海氷は 地球規模の気候システムの 重要な構成要素です

研究 の 目的:

  • 北極海氷の段階的な変化を特定し分析する.
  • 観測された変化における海氷の滞在時間の役割を調査する.

主な方法:

  • フラム海峡の海氷の継続的なモニタリングは 30年以上続いています
  • 海氷の厚さと変形データを分析した.
  • ダイナミックな海氷の濃縮過程のモデル化

主要な成果:

  • 2007年に北極海の氷が大きく変化し 厚くて変形した氷から 薄くて均一な氷へと変化しました
  • 厚く変形した氷の分子は 移転後半分に減り 回復していない.
  • 北極の海氷の滞在時間は2005年と2007年に2段階縮小されました

結論:

  • 観測された北極海氷の薄まりは,海氷の滞在時間が短縮されたことによって説明されます.

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Removal of Exogenous Materials from the Outer Portion of Frozen Cores to Investigate the Ancient Biological Communities Harbored Inside
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Removal of Exogenous Materials from the Outer Portion of Frozen Cores to Investigate the Ancient Biological Communities Harbored Inside

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Author Spotlight: Unveiling Plankton Response to Climate Change Through Time-Series Data and Artistic Expression
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Removal of Exogenous Materials from the Outer Portion of Frozen Cores to Investigate the Ancient Biological Communities Harbored Inside
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Removal of Exogenous Materials from the Outer Portion of Frozen Cores to Investigate the Ancient Biological Communities Harbored Inside

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  • 気候変動は北極の海氷の動態に 持続的な影響を及ぼしています
  • 発見は北極海氷の変化と 海洋海氷のプロセスとの関連を強調しています