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Global Climate Change01:50

Global Climate Change

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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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Effect of Sea Water on Concrete01:22

Effect of Sea Water on Concrete

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Concrete exposed to seawater can undergo degradation like the dissolution of ettringite and gypsum, increasing the material's porosity and decreasing its strength. In contrast, the crystallization of salts within the concrete's pores can cause expansion, particularly above the waterline where evaporation occurs. Nonetheless, this expansion only happens when seawater, enabled by the concrete's permeability, manages to infiltrate the structure.
Concrete in areas between tide marks,...
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Precipitation Gravimetry01:03

Precipitation Gravimetry

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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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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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Temperature Dependent Deformation01:12

Temperature Dependent Deformation

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In a nonhomogeneous rod made up of steel and brass, restrained at both ends and subjected to a temperature change, several steps are involved in calculating the stress and compressive load. Due to the problem's static indeterminacy, one end support is disconnected, allowing the rod to experience the temperature change freely. Next, an unknown force is applied at the free end, triggering deformations in the rod's steel and brass portions. These deformations are then calculated and added...
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Updated: Mar 17, 2026

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
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Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt

Published on: August 7, 2017

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"海底バチメトリーの気象による気象変動に対する感受性"に関するコメント

Maya Tolstoy1

  • 1Department of Earth and Environmental Sciences, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA.

Science (New York, N.Y.)
|July 16, 2016
PubMed
まとめ

ミランコビッチ周期は海底のバチメトリーで新しい発見によって支持されています. これらの地質信号を検出するのに最適の場所として特定されています.

科学分野:

  • 地理学
  • 海洋学
  • 気候科学

背景:

  • 最近の研究では,海底のバチメトリーデータ内のミランコビッチ周期の発見が報告されています.
  • オリーブらによるこれらの最初の発見に関して懸念と批判が提起された. そしてゴフ

研究 の 目的:

  • ミランコビッチサイクルについて提起された懸念に対処するために
  • これらのサイクルを観察するための重要な領域として,南東太平洋上昇を評価する.

主な方法:

  • 海底のバチメトリーデータ分析
  • 観測データと予測モデルの比較

主要な成果:

  • 批判にも関わらず,この研究の結果はミランコビッチサイクルの検出のための南東太平洋上昇の重要性を強化しています.
  • モデルはこの地域の観測されたバチメトリックデータと密接に一致しています.

結論:

  • 南東太平洋上昇は,海底の地形におけるミランコビッチサイクルを調査するための主要な場所です.
  • これらの発見は,海洋地質学的記録におけるこれらの長期的な気候強制信号の存在と検出可能性を裏付けています.

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