(Askeri) TROPOSFER: Yükseklikle ilgili ısı değişiminin nispi olarak fazla olduğu atmosferin alt katmanları. Bulutların oluştuğu, konveksiyonun faal olduğu ve karışımın sürekli olup, az ya da çok tam olduğu bir bölgedir. Ayrıca bakınız: "atmosphere"
Английский Язык - Английский Язык
Определение tropospheres в Английский Язык Английский Язык словарь
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 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 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 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 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
The lowest layer of the atmosphere The troposphere has distinctive winds and cloud formations, and it has a very marked drop in temperature with altitude It is 10 - 16 km from the surface of the Earth
Lowest region of the atmosphere, bounded by the Earth below and the stratosphere above, with the upper boundary being about 6-8 mi (10-13 km) above the Earth's surface. The troposphere is marked by decreasing temperature with height, which distinguishes it from the stratosphere. Most clouds and weather systems occur in the troposphere
The lower regions of a planetary atmosphere where convection keeps the gas mixed and maintains a steady increase of temperature with depth Most clouds are in the troposphere
The lowest layer of the atmosphere marked by considerable turbulence and a decrease in temperature with height This layer stretches from the surface to approximately 10km Weather on earth is created here