タグ

対流圏

10 件の記事

Comparison of the 1962 US Standard Atmosphere graph of geometric altitude against air density, pressure, the speed of sound and temperature with approximate altitudes of various objects.[1]

大気温度のメカニズム高度による変化と地表の温度変動

大気温度対流圏成層圏中間圏
The atmospheric gases around Earth scatter blue light (shorter wavelengths) more than light toward the red end (longer wavelengths) of the visible spectrum; thus, a blue glow over the horizon is seen when observing Earth from outer space. The Moon is visible in the background.

惑星大気のメカニズム組成から構造、宇宙への散逸まで

惑星大気天文学大気組成外惑星
Composition of the atmosphere of Venus. The chart on the right is an expanded view of the trace elements that all together do not even make up a tenth of a percent.

金星の大気構造と過酷な環境のメカニズム

金星大気組成二酸化炭素温室効果
Composition of the atmosphere of Venus. The chart on the right is an expanded view of the trace elements that all together do not even make up a tenth of a percent.

金星の大気構造極限環境の化学とダイナミクス

金星大気組成二酸化炭素硫酸雲
Earth's atmosphere from space, showing a blue layer at the stratosphere, above the clouds of the troposphere. The Moon is visible as a crescent in the background.[1]

地球の大気生命を育む多層構造とその役割

地球の大気対流圏成層圏中間圏
Earth's atmosphere from space, showing a blue layer at the stratosphere, above the clouds of the troposphere. The Moon is visible as a crescent in the background.[1]

地球の大気生命を育む多層構造とそのメカニズム

地球の大気対流圏成層圏中間圏
Satellite animation of the initial eruption column and shockwave from Hunga Tonga–Hunga Haʻapai on 15 January 2022

噴火柱のメカニズムと地球環境への影響

噴火柱火山噴火テフラ成層圏
A picture of Earth's troposphere with its different cloud types of low to high altitudes casting shadows. Sunlight is reflected off the ocean, after it was filtered into a reddish light by passing through much of the troposphere at sunset. The above lying stratosphere can be seen at the horizon as a band of its characteristic glow of blue scattered sunlight.

対流圏の仕組みと地球環境への影響

対流圏大気構造対流圏界面気温減率
Earth's atmosphere from space, showing a blue layer at the stratosphere, above the clouds of the troposphere. The Moon is visible as a crescent in the background.[1]

地球の大気生命を育む多層構造とそのメカニズム

地球の大気対流圏成層圏中間圏
Polar vortex and weather impacts due to stratospheric warming[clarification needed]

極渦(ポーラーボルテックス)の仕組みと気象への影響

極渦ポーラーボルテックス成層圏対流圏