FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2033439113> ?p ?o ?g. }

• W2033439113 endingPage "322" @default.
• W2033439113 startingPage "306" @default.
• W2033439113 abstract "Numerical time integrations of a nine-layer, quasi-geostrophic, highly truncated spectral model of the atmosphere are used to study tropospheric-stratospheric interaction with particular regard to sudden stratospheric warmings. The model is global, extends to 0.05 mb (71 km) with roughly 10-km resolution in the stratosphere, and includes an annual heating cycle. Model integrations simulating the months of December and January were made (1) without nonzonal forcing and (2) with nonzonal heating and orography included, to represent Southern Hemisphere and Northern Hemisphere winters, respectively. The presence of nonzonal heating in the winter hemisphere brought about an increase in circulation intensity and produced a stationary perturbation having a strong westward slope with height extending high into the stratosphere. This feature is similar to the Aleutian system. It was accompanied by considerably warmer temperatures in the polar night stratosphere and a weaker stratospheric westerly jet. Sudden stratospheric warmings occurred as a result of large increases in the intensity of planetary scale waves in the troposphere, which in turn produced surges of upward propagating energy. The energetics of the warming occurred in two phases. A change from a baroclinically direct to a driven circulation occurred as the stratospheric temperature gradient reversed. This coincided with a change from enhancement to absorption of the vertical energy flux. The mechanism of the warming was similar to that described by Matsuno. Nonlinear interactions between the progressive long wave and the nonzonal heating were primarily responsible for the tropospheric events that produced the transient upward flux of energy and thus the warmings. A seasonally coupled index cycle in the long waves was also of significance, while interactions with other waves and orographic forcing were of secondary importance in the long-wave energetics of sudden warmings." @default.
• W2033439113 created "2016-06-24" @default.
• W2033439113 creator A5031584459 @default.
• W2033439113 date "1973-04-01" @default.
• W2033439113 modified "2023-09-25" @default.
• W2033439113 title "Dynamic Coupling of the Stratosphere With the Troposphere and Sudden Stratospheric Warmings" @default.
• W2033439113 cites W1634556243 @default.
• W2033439113 cites W1665874614 @default.
• W2033439113 cites W1965651709 @default.
• W2033439113 cites W1970509591 @default.
• W2033439113 cites W1976223082 @default.
• W2033439113 cites W1988854175 @default.
• W2033439113 cites W1990405060 @default.
• W2033439113 cites W1996719859 @default.
• W2033439113 cites W1998247543 @default.
• W2033439113 cites W2004896601 @default.
• W2033439113 cites W2008082530 @default.
• W2033439113 cites W2009332505 @default.
• W2033439113 cites W2013580363 @default.
• W2033439113 cites W2013636535 @default.
• W2033439113 cites W2016181239 @default.
• W2033439113 cites W2022337564 @default.
• W2033439113 cites W2027491175 @default.
• W2033439113 cites W2030103095 @default.
• W2033439113 cites W2030456534 @default.
• W2033439113 cites W2031042760 @default.
• W2033439113 cites W2033039490 @default.
• W2033439113 cites W2038137915 @default.
• W2033439113 cites W2044456125 @default.
• W2033439113 cites W2050505450 @default.
• W2033439113 cites W2052554358 @default.
• W2033439113 cites W2053257456 @default.
• W2033439113 cites W2057030340 @default.
• W2033439113 cites W2062164891 @default.
• W2033439113 cites W2062909504 @default.
• W2033439113 cites W2065483077 @default.
• W2033439113 cites W2067324954 @default.
• W2033439113 cites W2075519947 @default.
• W2033439113 cites W2075776171 @default.
• W2033439113 cites W2080783784 @default.
• W2033439113 cites W2083387623 @default.
• W2033439113 cites W2084423060 @default.
• W2033439113 cites W2086304817 @default.
• W2033439113 cites W2093374886 @default.
• W2033439113 cites W2095204808 @default.
• W2033439113 cites W2095543252 @default.
• W2033439113 cites W2118127161 @default.
• W2033439113 cites W2126307584 @default.
• W2033439113 cites W2129240716 @default.
• W2033439113 cites W2137316144 @default.
• W2033439113 cites W2140281615 @default.
• W2033439113 cites W2146251153 @default.
• W2033439113 cites W2146692898 @default.
• W2033439113 cites W2173151082 @default.
• W2033439113 cites W2178910930 @default.
• W2033439113 cites W2605621984 @default.
• W2033439113 cites W2606271707 @default.
• W2033439113 cites W2607034238 @default.
• W2033439113 cites W3109198941 @default.
• W2033439113 cites W2345459192 @default.
• W2033439113 doi "https://doi.org/10.1175/1520-0493(1973)101<0306:dcotsw>2.3.co;2" @default.
• W2033439113 hasPublicationYear "1973" @default.
• W2033439113 type Work @default.
• W2033439113 sameAs 2033439113 @default.
• W2033439113 citedByCount "17" @default.
• W2033439113 countsByYear W20334391132019 @default.
• W2033439113 crossrefType "journal-article" @default.
• W2033439113 hasAuthorship W2033439113A5031584459 @default.
• W2033439113 hasBestOaLocation W20334391131 @default.
• W2033439113 hasConcept C121332964 @default.
• W2033439113 hasConcept C125405218 @default.
• W2033439113 hasConcept C127313418 @default.
• W2033439113 hasConcept C142756592 @default.
• W2033439113 hasConcept C153294291 @default.
• W2033439113 hasConcept C163861444 @default.
• W2033439113 hasConcept C2777882148 @default.
• W2033439113 hasConcept C2778835443 @default.
• W2033439113 hasConcept C39432304 @default.
• W2033439113 hasConcept C49204034 @default.
• W2033439113 hasConcept C53631411 @default.
• W2033439113 hasConcept C65440619 @default.
• W2033439113 hasConcept C88582754 @default.
• W2033439113 hasConcept C9075549 @default.
• W2033439113 hasConcept C91586092 @default.
• W2033439113 hasConceptScore W2033439113C121332964 @default.
• W2033439113 hasConceptScore W2033439113C125405218 @default.
• W2033439113 hasConceptScore W2033439113C127313418 @default.
• W2033439113 hasConceptScore W2033439113C142756592 @default.
• W2033439113 hasConceptScore W2033439113C153294291 @default.
• W2033439113 hasConceptScore W2033439113C163861444 @default.
• W2033439113 hasConceptScore W2033439113C2777882148 @default.
• W2033439113 hasConceptScore W2033439113C2778835443 @default.
• W2033439113 hasConceptScore W2033439113C39432304 @default.
• W2033439113 hasConceptScore W2033439113C49204034 @default.
• W2033439113 hasConceptScore W2033439113C53631411 @default.
• W2033439113 hasConceptScore W2033439113C65440619 @default.
• W2033439113 hasConceptScore W2033439113C88582754 @default.
• W2033439113 hasConceptScore W2033439113C9075549 @default.

• next