troposphäre (unterste schicht der erdatmosphäre)

Almanca - İngilizce

troposphäre (unterste schicht der erdatmosphäre) teriminin Almanca İngilizce sözlükte anlamı

troposphere

The lower levels of the atmosphere extending from the earth's surface up to the tropopause. It is characterized by convective air movements and a large vertical temperature change

That portion of the atmosphere from the earth's surface to the stratosphere; that is, the lowest 10 to 20 kilometers of the atmosphere The troposphere is characterized by decreasing temperature with height, appreciable vertical wind motion, appreciable water vapor content, and weather Dynamically, the troposphere can be divided into the following layers: surface boundary layer, Ekamn layer, and free atmosphere See atmospheric shell

The inner layer of the atmosphere below about 15 km, within which there is normally a steady decrease of temperature with increasing altitude Nearly all clouds form and weather conditions manifest themselves within this region, and its thermal structure is caused primarily by the heating of the Earth's surface by solar radiation, followed by heat transfer by turbulent mixing and convection (Source: Carbon Dioxide Information Analysis Center, 1990)

The portion of the atmosphere that is below the stratosphere It extends outward about 7 to 10 miles from the earth's surface

The lowest layer of the atmosphere

the portion of the earth's atmosphere from the surface to the tropopause; that is, the lowest 10-20 km of the atmosphere The troposphere is characterized by decreasing temperature with height, and is the layer of the atmosphere containing most clouds and other common weather phenomena

The lower atmosphere, from the earth's surface to approximately 12 km This portion of the earth's atmosphere contains about 95 percent of the atmospheric gases The temperature gradually declines through this region

The layer of the atmosphere lying below 10 km altitude More information here

The lowest region of the Earth's atmosphere, from ground level to the tropopause, where the temperature gradient goes to zero (height about 15 km) The troposphere is the region where most weather occurs

the lowest region of the atmosphere between the surface of the earth and the stratosphere In the troposphere the temperature usually decreases with increasing altitude

The lower levels of the atmosphere extending from the earths surface up to the tropopause. It is characterized by convective air movements and a large vertical temperature change

-Area of the earth's atmosphere extending from the surface of the earth up to the borders of the stratosphere, which is about 15 km above the earth This is the area in which we live, and all of the weather takes place The troposphere becomes increasingly colder the higher up you go, until the tropopause (the boundary between the troposphere and the stratosphere) is reached

Layer in the atmosphere found from the surface to approximately 11 kilometers of altitude This layer contains about 75 % of the total mass of the atmosphere It is also the layer where the majority of our weather occurs Maximum air temperature occurs near the Earth's surface in this layer With increasing altitude air temperature drops uniformly with increasing height at an average rate of 6 5 degrees Celsius per 1000 meters (commonly called the Environmental Lapse Rate), until an average temperature of -55 degrees Celsius is reached at the top of the troposphere

The lowest layer of the Earth's atmosphere, extending from the ground to the stratosphere at approximately 13 km of altitude In the troposphere, temperature decreases with height

The lowest part of the atmosphere The troposphere extends from the surface up to about 10 km in altitude, although this height varies with latitude Almost all weather takes place in the troposphere Mt Everest, the highest mountain on Earth, is only 8 8 km high Temperatures decrease with altitude in the troposphere As warm air rises it cools, falling back to Earth This process, known as convection, means there are huge air movements that mix the troposphere very efficiently

the layer of the atmosphere nearest the earth's surface The troposphere extends outward about 5 miles at the poles and 10 miles at the equator

The region of a planetary atmosphere nearest the surface, having a more or less uniform decrease of temperature with altitude In the Earth's atmosphere the nominal rate of temperature decrease is 6 5°K/km but inversions are common The troposphere, the domain of weather, is in convective equillibrium with the sun-warmed surface of the Earth

The layer of the atmosphere from the surface to where the temperature stops decreasing with height

The lowest layer of the atmosphere located between the earth's surface to approximately 11 miles (17 kilometers) into the atmosphere Characterized by clouds and weather, temperature generally decreases with increasing altitude

The region of the atmosphere, immediately above the earth's surface and up to the tropopause, in which the temperature falls fairly regularly with increasing altitude, clouds form, convection is active, and mixing is continuous and more or less complete