(Askeri) TROPOPAUSE: Stratosfer ile troposfer arasındaki bir geçiş bölgesi. Tropopause, kutup ve ılıman bölgelerde 25.000 ile 45.000 fit irtifada, tropik bölgelerde ise 55.000 fit yükseklikte oluşmaktadır. Ayrıca bak. "atmosphere"
Englisch - Englisch
Definition von tropopause im Englisch Englisch wörterbuch
The zone of transition between the troposphere and the stratosphere (approximately 13 kilometers). The tropopause normally occurs at an altitude of between 25,000 and 45,000 feet in polar and temperate zones. It occurs at 55,000 feet in the tropics
The narrow region separating the troposphere and the stratosphere More information here
The upper region of the troposphere In the Earth's atmosphere, the tropopause occurs between altitudes of about 6 to 18 kilometers and is the domain of high winds and highest cirrus clouds
The upper boundary of the troposphere, usually characterized by an abrupt change in lapse rate from positive (decreasing temperature with height) to neutral or negative (temperature constant or increasing with height) See Fig 6, sounding
The boundary between the upper troposphere and the lower stratosphere that varies in altitude from approximately 8 kilometers (5 miles) at the poles to approximately 18 kilometers (11 miles) at the equator back
The boundary zone or transition layer between the troposphere and the stratosphere This is characterized by little or no increase or decrease in temperature or change in lapse rate with increasing altitude
The boundary between the troposphere and stratosphere, usually characterized by an abrupt change of lapse rate The change is in the direction of increased atmospheric stability from regions below to regions above the tropopause Its height varies from 15 to 20 kilometers in the tropics to about 10 kilometers in polar regions In polar regions in winter it is often difficult or impossible to determine just where the tropopause lies, since under some conditions there is no abrupt change in lapse rate at any height
the boundary between the troposphere and stratosphere, characterized by an abrupt change in temperature lapse rate (temperatures decrease with height in the troposphere, but increase or remain constant with height in the stratosphere)
The zone of transition between the troposphere and the stratosphere (approximately 13 kilometers) The tropopause normally occurs at an altitude of between 25,000 and 45,000 feet in polar and temperate zones It occurs at 55,000 feet in the tropics
The imaginary boundary layer dividing the stratosphere from the lower part of the atmosphere, the troposphere The tropopause normally occurs at an altitude of about 25,000 to 45,000 feet in polar and temperate zones, and at 55,000 feet in the tropics See Stratosphere, Troposphere
The tropopause is an atmospheric layer that extends from approximately 11 to 20 kilometers above the Earth's surface In this layer temperature remains constant (isothermal) It is also the layer in the atmosphere where the jet stream exists
The boundary between the troposphere and the stratosphere (about 8 km in polar regions and about 15 km in tropical regions), usually characterized by an abrupt change of lapse rate The regions above the troposphere have increased atmospheric stability than those below The tropopause marks the vertical limit of most clouds and storms (Source: Carbon Dioxide Information Analysis Center, 1990)
The boundary between the troposphere and stratosphere, usually characterized by an abrupt change in lapse rate Its height varies from 10 to 20 km Regions above the tropopause have greater atmospheric stability than regions below