全球陆地季风系统的超级周期
1Laboratory for Climate and Ocean-Atmosphere Studies, Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, China.
National science review
|April 18, 2024
概括
全球陆地季风周期在面积和降雨强度方面显示出超级周期. 这种周期性与地质时间尺度上的超大陆周期密切相关.
科学领域:
- 古气候学 古气候学
- 地力学是什么?地力学是什么?
- 地球系统科学 地球系统科学
背景情况:
- 全球陆地季风系统在地质时间内表现出显著的变化.
- 了解季风强度和范围的驱动因素对于重建过去的气候至关重要.
研究的目的:
- 研究全球陆地-季风系统的长期周期性.
- 为了确定季风行为和超大陆配置之间的关系.
主要方法:
- 分析古气候代理数据以重建季风强度和面积.
- 季风超级周期和超级大陆周期之间的相关性分析.
主要成果:
- 全球陆地季风系统在整个法内罗纪时期的空间范围和降雨强度都显示出超级周期.
- 季风超级周期的时间与超级大陆周期之间存在很强的相关性.
结论:
- 大陆结构在管理全球陆地-季风系统方面发挥着主导作用.
- 季风的行为与构造过程和超大陆在地质时间尺度上的组装/解体密切相关.
更多相关视频
10:28Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
Published on: June 13, 2020
5.8K
09:55Surface Renewal: An Advanced Micrometeorological Method for Measuring and Processing Field-Scale Energy Flux Density Data
Published on: December 12, 2013
8.7K
相关概念视频
The Water Cycle
24.4K
The Earth’s hydrosphere includes all of the areas where the storage and movement of water occurs. Since water is the basis of all living processes, the cycling of water is extremely important to ecosystem dynamics.
24.4K
Global Climate Change
24.3K
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.
24.3K
What is Climate?
18.4K
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.
18.4K
The Carbon Cycle
37.4K
Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
37.4K
What are Biogeochemical Cycles?
31.6K
The most common elements in organic molecules, carbon, hydrogen, oxygen, nitrogen, sulfur, and phosphorus, are only available in the ecosystem in limited amounts. Therefore, these nutrients must be recycled through both biotic and abiotic components of the ecosystem, in processes generally called biogeochemical cycles.
31.6K
The Nitrogen Cycle
52.1K
Nitrogen atoms, present in all proteins and DNA, are recycled between abiotic and biotic components of the ecosystem. However, the primary form of nitrogen on Earth is nitrogen gas, which cannot be used by most animals and plants. Thus, nitrogen gas must first be converted into a usable form by nitrogen-fixing bacteria before it can be cycled through other living organisms. The use of nitrogen-containing fertilizers and animal waste products in human agriculture has greatly influenced the...
52.1K
