オーログラフィによる北米モンスーンの機械的強制
William R Boos1,2, Salvatore Pascale3,4
1Department of Earth and Planetary Science, University of California, Berkeley, CA, USA. billboos@alum.mit.edu.
Nature
|November 25, 2021
まとめ
北米のモンスーン
科学分野:
- 大気科学
- 気象学
- 気候の動態
背景:
- 北米のモンスーンはメキシコの西海岸に激しい降雨をもたらします.
- その駆動メカニズムは,伝統的に熱力強引に起因するが,これは議論されている.
研究 の 目的:
- 北米のモンスーンを駆動する 根本的なメカニズムを調査するために
- モンスーンの発展における陸地と大気の相互作用と山脈の役割を決定する.
主な方法:
- 大気動力学と熱力学に関する観測データの分析.
- グローバル気候モデルのシミュレーションを用いて
- アディアバティック静止波の溶液を適用する
主要な成果:
- シエラ・マドレ山脈は 熱帯圏外のジェットストリームを 機械的に赤道に押し寄せるのです
- この相互作用により 上昇の流れが生み出され,湿気が上昇し,コンベクティブの降雨が起こります
- 地表の熱流は,大気の予備条件付けで二次的な役割を果たします.
結論:
- 北米のモンスーンは主にコンベクティブにより強化されたオログラフィの降雨であり,典型的な熱的に強制された熱帯モンスーンではありません.
- ジェットストリームとオーログラフィーの相互作用は,モンスーンのダイナミクスにとって極めて重要です.
- これらのメカニズムの理解は 気候変動に対するモンスーンの反応を 予測するのに不可欠です
さらに関連する動画
06:55Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
Published on: August 5, 2016
8.3K
08:09Measuring and Mapping Patterns of Soil Erosion and Deposition Related to Soil Carbonate Concentrations Under Agricultural Management
Published on: September 12, 2017
12.0K
関連する概念動画
Coriolis Force
4.5K
An accelerating particle experiences a force equal to the mass multiplied by the acceleration in an inertial frame of reference. Consider a particle in a non-inertial frame of reference, such as a sliding ball on a rotating table. The acceleration of the ball in this rotating reference frame is different than in the intertial frame, which modifies its equation of motion. The fictitious forces acting additionally on a rotating frame of reference alter Newton's Second Law expression.
4.5K
Variation of Atmospheric Pressure
3.1K
Change in atmospheric pressure with height is particularly interesting. The decrease in atmospheric pressure with increasing altitude is due to the decreasing gravitational force per unit area as we move away from the surface of the earth.
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
Let p(y) be the atmospheric pressure at...
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
Let p(y) be the atmospheric pressure at...
3.1K
Precipitation Processes
693
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...
693
Tidal Forces
2.8K
The origin of Earth's ocean tides has been a subject of continuous investigation for over 2000 years. However, the work of Newton is considered to be the beginning of the proper understanding of the phenomenon. Ocean tides are the result of gravitational tidal forces. These same tidal forces are present in any astronomical body; they are responsible for the internal heat that creates the volcanic activity on Io, one of Jupiter's moons, and the breakup of stars that get too close to...
2.8K
What is Climate?
19.4K
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.
19.4K
Magnetostatic Boundary Conditions
1.2K
An electric field suffers a discontinuity at a surface charge. Similarly, a magnetic field is discontinuous at a surface current. The perpendicular component of a magnetic field is continuous across the interface of two magnetic mediums. In contrast, its parallel component, perpendicular to the current, is discontinuous by the amount equal to the product of the vacuum permeability and the surface current. Like the scalar potential in electrostatics, the vector potential is also continuous...
1.2K
