Cold air at the top of ascending columns is forced to one side by warmer air continuing to flow up from beneath but it is blocked by
the warmer stratospheric air above and so flows laterally and downward to the top of descending columns, following the undulating slope of the tropopause.
Not exact matches
Besides SSCE, scientists have also been investigating
stratospheric sulfur injections — firing sun - reflecting aerosols into the
air, similar to the cooling effect after a volcanic eruption — and cirrus cloud thinning, where you thin the top level of clouds, which have a
warming effect on the planet.
The
stratospheric sudden
warming events analyzed in the paper are driven by
air waves traveling upward from the troposphere — «so one could argue whether or not the troposphere is the primary cause of events,» Reichler says.
After it reaches streams and oceans, nitrogen molecules contribute to algal blooms and return to the
air to
warm the atmosphere and deplete
stratospheric ozone.
The Montreal Protocol had no impact on cleaning the
air, it stopped the growth of CFCs which are powerful greenhouse gases (in addition to their role in depleting
stratospheric ozone), therefore it slowed global
warming, rather than increasing it, and we aren't trying to save ground - level ozone.
Whilst flowing across the area between the two columns that cold
air does not
warm up by compression despite falling in height because it remains in contact with
stratospheric air with which it can freely exchange energy by conduction and mixing.
The Arctic surface
air temperature is strongly effected by atmospheric forcing and atmospheric energy circulated poleward which creates the Arctic Winter
Warming and Sudden Stratospheric warming
Warming and Sudden
Stratospheric warming warming events.
Hypothetically (and the relationship is already well established statistically) the gamut of Mid Winter
Warmings, Sudden
Stratospheric Warmings and Final
Warmings in the Arctic stratosphere depend upon the supply of ozone rich
air from mid latitudes being thrust into the Arctic stratosphere where ozone is normally in a somewhat depleted state due to erosive nitrogen compounds descending from the mesosphere, in turn related to Particle Precipitation Events that are strongly related to geomagnetic influences and the solar wind.
Erl on Feb 18, 15:03:07 «Sudden
stratospheric warmings in the Arctic depend upon the transport of ozone rich
air from above the Sea of Japan.
Sudden
stratospheric warmings in the Arctic depend upon the transport of ozone rich
air from above the Sea of Japan.
In addition, a phenomenon called sudden
stratospheric warming, apparently the result of strong downward
air motion, also occurs in the late winter and spring at high latitudes.
The
warm air intrusion followed two other related and noteworthy weather events, a sudden
warming of the stratosphere, known as a sudden
stratospheric warming event, and a splitting of the polar vortex.
(Any higher and they start to suffer
stratospheric heating due to the vertical temperature profile reversing at the tropopause — the lapse rate changes sign and the
air gets
warmer instead of colder with altitude.)
Posted by Neven on February 26, 2018 at 19:42 in AGW,
Air temperature, Arctic Basin, DMI, Greenland ice sheet, Records, Sudden
stratospheric warming, Uni Hamburg, WACC, Winter weirdness Permalink Comments (24)
But every two years on average, the
stratospheric air suddenly is disrupted and the vortex gets
warmer and weaker, and sometimes even shifts direction to clockwise.