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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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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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Threats to Biodiversity01:50

Threats to Biodiversity

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There have been five major extinction events throughout geological history, resulting in the elimination of biodiversity, followed by a rebound of species that adapted to the new conditions. In the current geological epoch, the Holocene, there is a sixth extinction event in progress. This mass extinction has been attributed to human activities and is thus provisionally called the Anthropocene. In 2019 the human population reached 7.7 billion people and is projected to comprise 10 billion by...
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Habitat Fragmentation02:31

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Habitat fragmentation describes the division of a more extensive, continuous habitat into smaller, discontinuous areas. Human activities such as land conversion, as well as slower geological processes leading to changes in the physical environment, are the two leading causes of habitat fragmentation. The fragmentation process typically follows the same steps: perforation, dissection, fragmentation, shrinkage, and attrition.
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Thermal Expansion01:22

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The expansion of alcohol in a thermometer is one of many commonly encountered examples of thermal expansion, which is the change in size or volume of a given system as its temperature changes. The most visible example is the expansion of hot air. When air is heated, it expands and becomes less dense than the surrounding air, which then exerts an upward force on the hot air to, for example, make steam and smoke rise, and hot air balloons float. The same behavior happens in all liquids and gases,...
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Population Growth00:57

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Population size is dynamic, increasing with birth rates and immigration, and decreasing with death rates and emigration. In ideal conditions with unlimited resources, populations can increase exponentially, which plots as a J-shaped growth rate curve of population size against time. This type of curve is characteristic of newly-introduced invasive species, or populations that have suffered catastrophic declines and are rebounding.
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Laser-Induced Fluorescence Emission L.I.F.E. as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats
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気候 変化 は 南極 の 氷 の ない 住居 の 拡大 を 促し て いる

Jasmine R Lee1,2, Ben Raymond3,4,5, Thomas J Bracegirdle6

  • 1Centre for Biodiversity and Conservation Science, School of Biological Sciences, The University of Queensland, Brisbane, Queensland 4072, Australia.

Nature
|June 29, 2017
PubMed
まとめ
この要約は機械生成です。

気候の変化により 南極の氷のない地域が大きく広がり 住環境の接続性が向上する可能性があります 生物の均質化と 独特の極地生態系での 種の消失につながる可能性があります

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科学分野:

  • 環境科学
  • 気候科学
  • エコロジー

背景:

  • 南極の陸上の生物多様性は,大陸の1%未満の氷のない地域に限定されています.
  • 気候変動はこれらの重要な生息地を変えると予測されていますが,その範囲と影響は不明です.

研究 の 目的:

  • 21世紀中に南極の氷のない地域に 気候変動の影響を定量化するためです
  • 気候変動のシナリオをモデル化する

主な方法:

  • 氷のない地域の変化をシミュレートするために,温度指数融解モデルを使用しました.
  • 気候変動に関する政府間パネル (IPCC) の2つの気候強制シナリオに基づく予測を分析した.

主要な成果:

  • 最も高い排出量のシナリオでは 氷のない面積は1万7千平方キロメートル増加し およそ25%増加する可能性があります
  • 南極半島では 氷のない地域を3倍に増やし 住環境の接続性を高めると予測されています

結論:

  • 南極の氷のない地域の増加は,生物多様性の生息地の利用可能性と接続性を変化させます.
  • 生物の均質化,競争力が低い種の絶滅,侵入種の広がりは 潜在的な結果である.