- Industry: Weather
- Number of terms: 60695
- Number of blossaries: 0
- Company Profile:
The American Meteorological Society promotes the development and dissemination of information and education on the atmospheric and related oceanic and hydrologic sciences and the advancement of their professional applications. Founded in 1919, AMS has a membership of more than 14,000 professionals, ...
実際に、土壌中の水の量と、土壌が保持できる水の量の差です。水、土壌が保持できる量一般に重力土壌孔隙から水を流出した後に残っている水の量はフィールドの容量と呼びます。フィールドの保水容量, 重力水を参照してください。
Industry:Weather
A downburst on the misoscale. Bow echoes are often associated with macrobursts. See also microburst.
Industry:Weather
バルーンを密封されていません。バルーンの基盤は開かれていることがあります。 または高ダクト バルーンまたはバルーンの基地の近くでに接続されている必要があります。開口部は、バルーンが天井高度に達すると過剰なガスを発散するため使用されます。高度 40 km 以上に科学的なペイロードを運ぶに使用される大規模なプラスチック製の風船がゼロ プレッシャー気球です。
Industry:Weather
A term used when the whole or a large part of a cloud undergoes a change from one genus to another. The new cloud is then given the name of the appropriate genus, followed by the name of the genus of the mother-cloud with the addition of the suffix “mutatus” (e. G. , stratus stratocumulomutatus). Compare genitus.
Industry:Weather
1. 衛星サブポイントは、衛星の直下を中心とした地球の表面に。これは地球軌道の衛星のゼロどん底角度のポイントとも呼ばれます。2. 特定のオブザーバーの天球、彼の天頂の正反対の点、オブザーバーのすぐ下。
Industry:Weather
A strong wind of monsoon origin that blows from between the northwest and north-northwest and sets in about the end of May or early June in the historic Seistan district of eastern Iran and Afghanistan. It continues almost without cessation until about the end of September. From its duration it is known as the wind of 120 days (bad-i-sad-o-bistroz). It sometimes reaches a velocity of more than 31 m s<sup>−1</sup> (70 mph) and carries much sand and dust. This sand blast is very erosive; buildings are eaten away and undercut near the ground. In some places the sand is deposited as wandering dunes, which overwhelm buildings and choke water supplies. All buildings in the region have blank walls on the windward side. The seistan is associated (along with the European etesians, and the shamal) with the deep summertime low over northwest India.
Industry:Weather
A strong wind of monsoon origin that blows from between the northwest and north-northwest and sets in about the end of May or early June in the historic Seistan district of eastern Iran and Afghanistan. It continues almost without cessation until about the end of September. From its duration it is known as the wind of 120 days (bad-i-sad-o-bistroz). It sometimes reaches a velocity of more than 31 m s<sup>−1</sup> (70 mph) and carries much sand and dust. This sand blast is very erosive; buildings are eaten away and undercut near the ground. In some places the sand is deposited as wandering dunes, which overwhelm buildings and choke water supplies. All buildings in the region have blank walls on the windward side. The seistan is associated (along with the European etesians, and the shamal) with the deep summertime low over northwest India.
Industry:Weather
