まとめ
北半球の降水量は,過去40年間にわたり,中緯度で大幅に増加し,低緯度で減少しています. これらの傾向は,炭素二酸化物の影響のみではなく,自然の気候の変動を反映しています.
科学分野:
- 気候学 気候学
- 大気科学 大気科学
- 環境科学 環境科学
背景:
- 長期の降水データは,気候の動態を理解する上で極めて重要です.
- 北半球の降雨パターンは顕著な変化を示しています.
研究 の 目的:
- 19世紀半ば以来,北半球の陸地における大規模な降水変化を調査するために.
- 半球と大陸のスケールにおける長期の降水変動を分析する.
主な方法:
- 歴史的な降水量測定の広範な配列を利用した.
- 19世紀半ばまで遡るデータを分析した.
主要な成果:
- 過去30~40年にわたって,中緯度の降雨量の有意な増加が観察されています.
- 同じ期間の低緯度の降雨量の同時減少が記録されている.
- 大気中の二酸化炭素濃度が倍増した際の観測された傾向と一般循環モデル予測の一貫性を指摘した.
結論:
- 観測された大規模な降雨傾向は,自然気候の変動性を示すものである.
- 地域差を精査し,データネットワークの不均一性に対処するためにさらなる研究が必要である.
- この研究は,気候変動を理解する上で長期的なデータの重要性を強調しています.
関連する概念動画
Precipitation and Co-precipitation
Precipitation and coprecipitation methods can be used to separate a mixture of ions in a solution. In qualitative inorganic analysis, ions that form sparingly soluble precipitates with the same reagent are separated based on the differences in solubility products. For example, consider the separation of Cu(II) and Fe(II) ions by precipitation as insoluble sulfides. First, copper(II) sulfide is precipitated by the addition of acidic H2S, where the dissociation of H2S is suppressed. Adding H2S...
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.
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.
Precipitation Processes
The experimental conditions in a gravimetric analysis should be optimized to maximize the particle size and purity of the obtained precipitate. Ideally, the concentration of the precipitating reagent should be low with effective stirring to maintain low relative supersaturation for the growth of large crystals. In homogeneous precipitation, the precipitant is slowly generated by a chemical reaction in the solution to avoid local reagent excesses. For example, urea decomposes gradually to...
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...
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...
What is Weather?
Overview

