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相关概念视频

States of Water01:23

States of Water

Water exists in any one of the three classical states: solid (ice), liquid (water), and gas (steam or water vapor). The state of water depends on i) the intermolecular forces that draw molecules together and ii) the kinetic energy that leads to movements that pull them apart.
Water freezes when the intermolecular forces are greater than the kinetic energy. Unlike most other substances, water is less dense in its solid state than in its liquid state. This is because each water molecule can form...
Optimal Foraging00:48

Optimal Foraging

How animals obtain and eat their food is called foraging behavior. Foraging can include searching for plants and hunting for prey and depends on the species and environment.
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Responses to Drought and Flooding02:41

Responses to Drought and Flooding

Water plays a significant role in the life cycle of plants. However, insufficient or excess of water can be detrimental and pose a serious threat to plants.
Marine Microbial Ecology01:30

Marine Microbial Ecology

Marine microbial ecosystems are shaped by distinct physicochemical limits, including high salinity, low nutrient availability, and fluctuating oxygen levels. These conditions favor smaller microbial cell sizes, which maximize their surface-to-volume ratio for efficient nutrient uptake.Microbial activity and community composition are closely linked to biogeochemical cycles, particularly in dynamic environments like estuaries, where halotolerant microbes thrive in response to variable salinity...
Deep Sea Microbial Ecology01:18

Deep Sea Microbial Ecology

The deep ocean and its underlying sediments represent vast, largely unexplored microbial habitats that extend far beyond the sunlit photic zone. The photic (euphotic) zone typically spans the upper ~100–200 meters of pelagic waters in the open ocean, but its depth varies geographically and seasonally, where sufficient light supports photosynthetic life. Below this lies the deep sea, spanning roughly 1000–6000 meters (bathypelagic to abyssal zones), with deeper hadal trenches extending beyond...

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Updated: Jul 12, 2026

An Ultra-clean Multilayer Apparatus for Collecting Size Fractionated Marine Plankton and Suspended Particles
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对于干旱而言,这是一个完美的海洋.

Martin Hoerling1, Arun Kumar

  • 1Climate Diagnostics Center, National Oceanic and Atmospheric Administration (NOAA), Boulder, CO 80305, USA. Martin.P.Hoerling@noaa.gov

Science (New York, N.Y.)
|February 1, 2003
PubMed
概括
此摘要是机器生成的。

1998年至2002年的全球干旱与持续的海洋温度有关. 气候模型揭示了协同作用的海洋影响,推动了广泛的中度干旱和同步干旱事件.

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科学领域:

  • 气候学 气候学 气候学
  • 海洋学 海洋学 海洋学
  • 干旱研究 干旱研究

背景情况:

  • 在1998年至2002年期间,美国,欧洲南部和西南亚经历了严重的干旱.
  • 在此期间,在关键的海洋地区观察到持续的异常海面温度 (SST).

研究的目的:

  • 调查1998-2002年广泛干旱背后的海洋共同驱动因素.
  • 了解不同海洋影响对中度干旱的协同作用.

主要方法:

  • 对1998-2002年海面温度 (SST) 数据的分析.
  • 利用气候模型模拟观察到的海洋条件对区域气候的影响.

主要成果:

  • 寒冷的东部热带太平洋SST和温暖的西部热带太平洋/印度洋SST持续存在.
  • 这些不同的海洋信号协同作用,有助于同步的中度干燥.
  • 印度洋和西太平洋海域前所未有的变暖与温室气体排放相结合.

结论:

  • 海洋影响在同步和加剧1998-2002年干旱方面发挥了关键作用.
  • 温室气体的排放可能导致了导致这些干旱的异常海洋温暖.
  • 这些发现对理解和预测未来的干旱事件有意义.