相关实验视频
Updated: May 21, 2025

06:27
Simulating Impacts of Ice Storms on Forest Ecosystems
Published on: June 30, 2020
6.9K
加大冬季北极变暖导致欧亚冷却通过非线性反被抑制的 synoptic eddy 活动
Manman Yin1, Xiu-Qun Yang1, Linyuan Sun1
1China Meteorological Administration Key Laboratory for Climate Prediction Studies, School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China.
Science advances
|March 19, 2025
概括
扩大北极变暖与较低的欧亚亚洲温度有关. 这项研究提供了证据表明,北极变暖事件通过抑制天气干扰,创造双极模式,导致欧亚冷却.
科学领域:
- 气候学 气候学 气候学
- 大气科学 大气科学
- 北极研究研究北极研究
背景情况:
- 近几十年来,北极的冬季变暖加速.
- 北极变暖和欧亚冷却之间的因果关系受到争论.
研究的目的:
- 提供北极变暖对欧亚大陆温度的影响的直接观测证据.
- 阐明将北极变暖与欧亚冷却联系在一起的机制.
主要方法:
- 识别每日北极变暖事件的情况.
- 在欧亚大陆上对天气干扰 (同视) 活动的分析.
- 对地势高度异常和反机制的调查.
主要成果:
- 直接的观测证据表明,北极的变暖导致欧亚大陆大幅降温,延迟约2天.
- 北极的变暖抑制了欧亚大陆高度地区的同视活动.
- 一个双极模式的地势高度异常出现,导致欧亚冷却通过冷向导.
结论:
- 温暖的北极 - 寒冷的欧亚大陆现象是一个内在的二极体,由同光学 - 平均流相互作用驱动.
- 北极变暖通过大气动力学直接影响欧亚大陆的天气模式.
相关概念视频
Global Climate Change
24.0K
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.
24.0K
Threats to Biodiversity
22.0K
There have been five major extinction events throughout geological history, resulting in the elimination of biodiversity, followed by a rebound of species that adapted to the new conditions. In the current geological epoch, the Holocene, there is a sixth extinction event in progress. This mass extinction has been attributed to human activities and is thus provisionally called the Anthropocene. In 2019 the human population reached 7.7 billion people and is projected to comprise 10 billion by...
22.0K
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
Joule-Thomson Effect
2.6K
The Joule-Thomson effect, also known as the Joule-Kelvin effect, describes the temperature change of a fluid when it is forced through a valve or porous plug while keeping it in a thermally insulated environment. This experiment is called a throttling process. This is an important effect widely used in refrigeration and the liquefaction of gases.
This experiment forces high-pressure gas through a throttle valve or a porous plug to a lower-pressure region. The gas expands as it passes through to...
This experiment forces high-pressure gas through a throttle valve or a porous plug to a lower-pressure region. The gas expands as it passes through to...
2.6K
Phase Transitions: Melting and Freezing
12.2K
Heating a crystalline solid increases the average energy of its atoms, molecules, or ions, and the solid gets hotter. At some point, the added energy becomes large enough to partially overcome the forces holding the molecules or ions of the solid in their fixed positions, and the solid begins the process of transitioning to the liquid state or melting. At this point, the temperature of the solid stops rising, despite the continual input of heat, and it remains constant until all of the solid is...
12.2K
What is Climate?
18.1K
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.
18.1K

