熱帯の平均放射能エネルギー予算における10年ごとに大きな変動を示す証拠
Bruce A Wielicki1, Takmeng Wong, Richard P Allan
1NASA Langley Research Center, Hampton, VA 23681, USA. b.a.wielicki@larc.nasa.gov
まとめ
地球の熱帯放射能エネルギー予算は,雲の変化によって引き起こされる,想定以上に変動しています. 現在の気候モデルは,この変動を捉えることができず,よりよい気候予測のために,熱帯雲のモデリングを改良する必要が生じます.
科学分野:
- 気候科学 気候科学
- 大気物理学 大気物理学
- 地球システム科学 地球システム科学
背景:
- 地球の放射能予算は,大規模では安定していると考えられています.
- 以前の理解では,大気上の熱帯放射能エネルギー予算 (TOA) の変動は最小限であると示唆されていた.
研究 の 目的:
- TOAの熱帯放射能エネルギー予算の変動性を調査する.
- 観測された変動を気候モデルシミュレーションと比較する.
主な方法:
- 20年以上にわたる衛星データの分析.
- 気候モデルシミュレーションの結果の収集と検証.
主要な成果:
- TOAの熱帯放射能エネルギー予算は,これまで考えられていたよりもはるかにダイナミックな変動性を示しています.
- 観測された放射線予算の変化は,主に熱帯の平均曇りの変動に起因する.
- 現在の気候モデルは,熱帯エネルギー予算の観測された大きな変動を誤って予測しています.
結論:
- 熱帯の曇りは,地球のエネルギー予算を調節する上で重要な役割を果たします.
- 気候モデルの中で,熱帯地域の雲のモデリングを強化する必要が非常に重要です.
- 改善された熱帯雲モデリングは,年間および十年間の熱帯気候変動のより正確な予測に不可欠です.
関連する概念動画
Trophic Efficiency
Trophic level transfer efficiency (TLTE) is a measure of the total energy transfer from one trophic level to the next. Due to extensive energy loss as metabolic heat, an average of only 10% of the original energy obtained is passed on to the next level. This pattern of energy loss severely limits the possible number of trophic levels in a food chain.
Energy Budgets and Reproductive Strategies
Organisms must balance energy intake with the energy required for growth, maintenance, and reproduction. These trade-offs result in a variety of survivorship and reproductive strategies, including semelparity and iteroparity. Semelparous species reproduce only once in their lifetime, often investing most available resources into that single reproductive event. Iteroparous species, by contrast, reproduce multiple times over their lifetimes, typically allocating fewer resources to any single...
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.
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.
Radiation: Applications
The average temperature of Earth is the subject of much current discussion. Earth is in radiative contact with both the Sun and dark space; it receives almost all its energy from the radiation of the Sun and reflects some of it into outer space. Dark space is very cold, about 3 K, so Earth radiates energy into it. For instance, heat transfer occurs from soil and grasses, the rate of which can be so rapid that frost can occur on clear summer evenings, even in warm latitudes.
The average...
The average...
Microbes and Climate Change
Microorganisms are pivotal agents in Earth's biogeochemical cycles, significantly influencing climate dynamics through their metabolic activities. These microbes modulate the levels of key greenhouse gases by both contributing to and helping mitigate climate change.Microbial Contributions to Greenhouse Gas EmissionsRising global temperatures accelerate microbial metabolism, which, in turn, speeds up the decomposition of organic matter. This process releases carbon dioxide (CO₂) through...


