まとめ
西南極の氷床は,西南極の氷床である.
科学分野:
- 氷河学と気候科学.
- 南極の研究と氷の動力学.
背景:
- 氷河流は,氷床の安定性の重要な構成要素である.
- 基礎条件を理解することは,氷床の振る舞いを予測する鍵です.
研究 の 目的:
- 西南極氷床の氷河流Bの基礎条件を調査する.
- 急速な氷河流の動きを駆動するメカニズムを決定する.
主な方法:
- 氷の底辺に穴を掘っている.
- 基礎水圧と温度を測定する.
主要な成果:
- 氷の底は,融解点にある.
- 基礎水圧は,過重圧に近い (1.6バー以内).
- 凝固していない堆積物の厚い層が氷の下にある.
結論:
- これらの基礎条件は,基礎滑りや沈殿物の変形を経由して,氷の急速な流れを促進します.
- 氷河流のメカニズムは,気候変動に対する氷床の反応を理解するために不可欠です.
関連する概念動画
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.
Frost Action on Concrete
Concrete structures in cold climates, such as those along roadsides, can retain moisture. This moisture makes them susceptible to frost-related damage when temperatures fall below freezing. Adding moisture worsens the damage during temperature fluctuations, leading to repeated freezing and thawing. De-icing salts, spread over these structures to melt ice, add to the freeze-thaw cycle, and draw even more moisture into the concrete.
This freeze-thaw cycle primarily causes surface scaling, where...
This freeze-thaw cycle primarily causes surface scaling, where...
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.
Conditions on Early Earth
Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
Conditions on Early Earth
Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
What is Weather?
Overview


