相关实验视频
Updated: May 22, 2025

06:27
Simulating Impacts of Ice Storms on Forest Ecosystems
Published on: June 30, 2020
6.9K
欧洲过去的极端水气候是由大西洋喷流和反复出现的天气模式驱动的
Stefan Brönnimann1,2, Jörg Franke1,2, Veronika Valler1,2
1Institute of Geography, University of Bern, Bern, Switzerland.
概括
大西洋喷流影响欧洲的天气. 它过去600年的变化,包括强度和位置,与干旱和洪水相关,但最近的变化是在自然历史范围之内.
科学领域:
- 大气科学 大气科学
- 气候科学 气候科学
- 古气候学 古气候学
背景情况:
- 大西洋喷流对欧洲的天气和气候产生重大影响,影响极端温度,水分传输和大气阻塞.
- 气候变化可能会改变喷流的特征,但其长期变化程度尚不清楚.
研究的目的:
- 分析大西洋 - 欧洲喷流在过去600年 (1421-2023) 的强度,倾斜和度的年间到十年间的变化.
- 调查喷流变化与欧洲干旱和洪水发生之间的关系.
主要方法:
- 利用了每月和每天大气场重建的集合来得出喷流指数.
- 与阻塞频率,旋风活动和干旱/洪水记录的历史数据进行比较.
主要成果:
- 一个向极移动的喷气流与中欧夏季干旱的加剧有关.
- 与减少阻塞相关的向赤道移动的喷气流与西欧和阿尔卑斯山的频繁冬季洪水有关.
- 火山爆发显著影响喷流的强度和倾斜.
- 最近的喷流指数变化属于过去六个世纪观察到的自然变化.
结论:
- 喷流的位置和强度是欧洲长期干旱和洪水模式的关键驱动因素.
- 最近洪水和干旱频率的增加并不能归因于喷流最近变化的变化.
- 火山活动对喷流动力学有着显著的影响.
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
What is Weather?
18.0K
Overview
18.0K
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
The Water Cycle
24.0K
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.
24.0K
Precipitation Processes
359
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...
359
Precipitation and Co-precipitation
1.6K
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...
1.6K

