地下海洋变异性在热带气旋起源中的关键作用
Cong Gao1,2, Lei Zhou3,4, I-I Lin5
1School of Oceanography, Shanghai Jiao Tong University, Shanghai, China.
Nature communications
|January 26, 2025
概括
地下海洋变化通过改变海洋热量含量,显著影响热带气旋的形成. 26°C等热深度的变化会影响海面温度,在全球范围内调节旋风的发展.
科学领域:
- 海洋学 海洋学 海洋学
- 气象学 天气学
- 气候科学 气候科学
背景情况:
- 热带气旋从上层海洋中吸取热能.
- 地下海洋动态对热带气候周期形成的影响仍然未得到充分研究.
研究的目的:
- 为了研究地下海洋变异性对热带气候周期发生的影响.
- 探索26°C同热深度在调节旋风形成中的作用.
主要方法:
- 分析海面风的压力和卷曲,以了解海洋内部的扰动.
- 评估26°C同热深度的波动及其对海洋热量含量的影响.
- 检查海面温度异常的诱导及其对热带气旋生成的调制.
主要成果:
- 地下海洋变化,特别是在26°C的同热深度,在全球范围内显著影响热带循环生成.
- 海洋内部被风应力和卷曲扰动到100米以上,导致深度波动.
- 在正在发展的旋风下调节的海面温度异常与这些地下变化有关.
结论:
- 地下海洋动力学在热带气候周期发生过程中起着至关重要的,以前被忽视的作用.
- 26°C同热深度的变化是影响旋风形成的关键驱动因素.
- 海洋内部变化和热带气旋的发展之间存在着意想不到的关系.
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
5.7K
13:27Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
Published on: June 8, 2015
8.7K
相关概念视频
Precipitation Processes
413
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...
413
The Water Cycle
24.1K
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.
24.1K
Precipitation Gravimetry
5.2K
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...
5.2K
Precipitation and Co-precipitation
1.7K
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...
1.7K
Isothermal Processes
3.5K
A thermodynamic process that occurs at constant temperature is called an isothermal process. Heat slowly flows into the system or out of the system to maintain thermal equilibrium. Processes involving phase changes like water evaporation into steam or freezing water into ice at a constant temperature are examples of Isothermal Processes.
An ideal gas can also undergo isothermal expansion or compression.
For example, consider 1 mole of an ideal gas inside an isolated cylinder at initial volume V...
An ideal gas can also undergo isothermal expansion or compression.
For example, consider 1 mole of an ideal gas inside an isolated cylinder at initial volume V...
3.5K
Boundary Layer Characteristics
28
When a fluid encounters a solid surface, a boundary layer forms due to the interaction between the fluid's motion and the stationary surface. This phenomenon is characterized by a thin region adjacent to the surface where viscous forces dominate, influencing the fluid's velocity profile. The development of the boundary layer begins at the leading edge of the surface and evolves as the fluid moves downstream.As the fluid flows over the surface, friction between the fluid and the wall slows down...
28
