stratosphere oor Noorweegse Nynorsk

stratosphere

naamwoord
en
(geology, obsolete) Collectively, those layers of the Earth’s crust which primarily comprise stratified deposits.

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stratosfære

naamwoordmanlike
en
region of the uppermost atmosphere
en.wiktionary2016

stratosfæren

naamwoord
en
layer of the atmosphere
wikidata

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The chemistry of the Antarctic polar vortex has created severe ozone depletion. The nitric acid in polar stratospheric clouds reacts with chlorofluorocarbons to form chlorine, which catalyzes the photochemical destruction of ozone.[39] Chlorine concentrations build up during the polar winter, and the consequent ozone destruction is greatest when the sunlight returns in spring.[40] These clouds can only form at temperatures below about −80 °C (−112 °F).
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Long-term cooling effects are primarily dependent upon injection of sulfide compounds in aerosol form into the upper atmosphere—the stratosphere—the highest, least active levels of the lower atmosphere where little precipitation occurs, thus requiring a long time to wash the aerosols out of the region.
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In the 1970s it was recognized by Richard Lindzen and James Holton that the periodic wind reversal was driven by atmospheric waves emanating from the tropical troposphere that travel upwards and are dissipated in the stratosphere by radiative cooling.
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The stratosphere is situated between about 10 km (6 mi) and 50 km (30 mi) altitude above the surface at moderate latitudes, while at the poles it starts at about 8 km (5 mi) altitude.
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The ozone layer is a layer of ozone high up in the Earth's atmosphere (stratosphere).
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The sulfate aerosols also promote complex chemical reactions on their surfaces that alter chlorine and nitrogen chemical species in the stratosphere.
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Under persistent condensation or deposition, cloud droplets or snowflakes form, which precipitate when they reach a critical mass. Increasing stratospheric water vapor at Boulder, Colorado.
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In the extreme cold of the polar winter, however, stratospheric clouds of different types may form, which are classified according to their physical state and chemical composition.
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Distribution in the mesosphere is similar to the stratosphere except at much higher altitudes.
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The QBO induces a secondary circulation that is important for the global stratospheric transport of tracers, such as ozone or water vapor.
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The projectile was the first human-made object to reach the stratosphere.
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The tropopause is between the troposphere and the stratosphere.
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The ozone layer or ozone shield is a region of Earth's stratosphere that absorbs most of the Sun's ultraviolet (UV) radiation.
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The tropopause is the boundary region between the troposphere and the stratosphere.
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Measuring the temperature change with height through the troposphere and the stratosphere identifies the location of the tropopause.
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The most significant impacts from these injections come from the conversion of sulfur dioxide to sulfuric acid (H2SO4), which condenses rapidly in the stratosphere to form fine sulfate aerosols.
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The stratosphere is very dry; unlike the troposphere, it rarely allows clouds to form.
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Atop the troposphere is the tropopause, which is the border between the troposphere and stratosphere.
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The tropopause is the boundary in the Earth's atmosphere between the troposphere and the stratosphere.
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For years after large Plinian eruptions, the blue cast of the sky is notably brightened by the persistent sulfate load of the stratospheric gases.
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Stratosphere measurements are conducted to measure ozone and UV levels, in particular to gain additional information about ozone depletion and the Antarctic ozone hole.
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In the stratosphere the temperature increases with altitude, and the stratopause is the region where a maximum in the temperature occurs.
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The injected ash also falls rapidly from the stratosphere; most of it is removed within several days to a few weeks.
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On Earth, a polar vortex is usually in the middle and upper troposphere and stratosphere. The cyclone surrounds the polar highs.
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A large number of minor and trace gases are also found in volcanic emissions, for example hydrogen, carbon monoxide, halocarbons, organic and pumice) into the stratosphere to heights of 16–32 kilometres (10–20 mi) above the Earth's surface.
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33 sinne gevind in 7 ms. Hulle kom uit baie bronne en word nie nagegaan nie.