mesopause वाक्य
उदाहरण वाक्य
मोबाइल
- Zambia; 7 . mesopause because it's not associated with Earth structure; 8.
- This results in a measurable effect-the mesopause should become cooler with increased CO 2.
- In recent years the mesopause has also been the focus of studies on global climate change associated with increases in CO 2.
- The upper boundary of the mesosphere is the mesopause, which can be the coldest naturally occurring place on Earth with temperatures below.
- Which of the following items does not belong on this list, and why : core, crust, mantle, mesopause, Moho?
- Observations do show a decrease of temperature of the mesopause, though the magnitude of this decrease varies and is subject to further study.
- Another feature is that the summer mesopause is cooler than the winter ( sometimes referred to as the " mesopause anomaly " ).
- Another feature is that the summer mesopause is cooler than the winter ( sometimes referred to as the " mesopause anomaly " ).
- The mesopause, at an altitude of, separates the mesosphere from the thermosphere & mdash; the second-outermost layer of the Earth's atmosphere.
- Air rising will expand and cool resulting in a cold summer mesopause and conversely downwelling air results in compression and associated increase in temperature at the winter mesopause.
- Air rising will expand and cool resulting in a cold summer mesopause and conversely downwelling air results in compression and associated increase in temperature at the winter mesopause.
- Just below the mesopause, the air is so cold that even the very scarce water vapor at this altitude can be sublimated into polar-mesospheric noctilucent clouds.
- In the second layer temperature starts to decrease again reaching about 165 K ( " 108 �C ) at the altitude of 95 km, where mesopause begins.
- The sodium emissions come from a thin sodium layer approximately 10 km thick at an altitude of 90 100 km, above the mesopause and in the D-layer of the ionosphere.
- The peak PMSE height is slightly below the summer mesopause temperature minimum at 88 km, and above the noctilucent cloud ( NLC ) and / or polar mesospheric cloud ( PMC ) layer at 83 84 km.
- To compute dust and smoke effects, they employed a one-dimensional microphysics / radiative-transfer model of the Earth's lower atmosphere ( to the mesopause ), which defined only the vertical characteristics of the global climate perturbation.
- In the dayside mesopause, which serves as a boundary between the mesophere and thermosphere and is located between 95 120 km, temperature increases to a constant about 300 400 K ( 27 127 �C ) value prevalent in the thermosphere.
- The exact upper and lower boundaries of the mesosphere vary with latitude and with season, but the lower boundary of the mesosphere is usually located at heights of about above the Earth's surface and the mesopause is usually at heights near, except at middle and high latitudes in summer where it descends to heights of about.
- The specific objectives of ISAMS were : ( i ) To obtain measurements of atmospheric temperature as a function of pressure, from the tropopause to the mesopause, with good accuracy and spatial resolution, and hence to study the structure and dynamics of the region, ( ii ) To investigate the distribution and variability of water vapour in the middle atmosphere, to determine its role in the atmospheric general circulation, and its sources and sinks in the middle atmosphere, ( iii ) To measure the global distribution of oxides of nitrogen and hence to investigate their origins and their roles in catalytic cycles which control the amount of ozone in the stratospheric ozone layer.
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