FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2259685131> ?p ?o ?g. }

• W2259685131 endingPage "560" @default.
• W2259685131 startingPage "541" @default.
• W2259685131 abstract "Abstract. Recent studies on the formation of a quasi-permanent layer of enhanced static stability above the thermal tropopause revealed the contributions of dynamical and radiative processes. Dry dynamics leads to the evolution of a tropopause inversion layer (TIL), which is, however, too weak compared to observations and thus diabatic contributions are required. In this study we aim to assess the importance of diabatic processes in the understanding of TIL formation at midlatitudes. The non-hydrostatic model COSMO (COnsortium for Small-scale MOdelling) is applied in an idealized midlatitude channel configuration to simulate baroclinic life cycles. The effect of individual diabatic processes related to humidity, radiation, and turbulence is studied first to estimate the contribution of each of these processes to the TIL formation in addition to dry dynamics. In a second step these processes are stepwise included in the model to increase the complexity and finally estimate the relative importance of each process. The results suggest that including turbulence leads to a weaker TIL than in a dry reference simulation. In contrast, the TIL evolves stronger when radiation is included but the temporal evolution is still comparable to the reference. Using various cloud schemes in the model shows that latent heat release and consecutive increased vertical motions foster an earlier and stronger appearance of the TIL than in all other life cycles. Furthermore, updrafts moisten the upper troposphere and as such increase the radiative effect from water vapor. Particularly, this process becomes more relevant for maintaining the TIL during later stages of the life cycles. Increased convergence of the vertical wind induced by updrafts and by propagating inertia-gravity waves, which potentially dissipate, further contributes to the enhanced stability of the lower stratosphere. Finally, radiative feedback of ice clouds reaching up to the tropopause is identified to potentially further affect the strength of the TIL in the region of the clouds." @default.
• W2259685131 created "2016-06-24" @default.
• W2259685131 creator A5032017067 @default.
• W2259685131 creator A5045109869 @default.
• W2259685131 creator A5054274097 @default.
• W2259685131 date "2016-01-19" @default.
• W2259685131 modified "2023-10-17" @default.
• W2259685131 title "The tropopause inversion layer in baroclinic life-cycle experiments: the role of diabatic processes" @default.
• W2259685131 cites W1619912090 @default.
• W2259685131 cites W1783612643 @default.
• W2259685131 cites W1974482615 @default.
• W2259685131 cites W1991089909 @default.
• W2259685131 cites W1997516735 @default.
• W2259685131 cites W2005904805 @default.
• W2259685131 cites W2011565179 @default.
• W2259685131 cites W2027573199 @default.
• W2259685131 cites W2036168723 @default.
• W2259685131 cites W2038742869 @default.
• W2259685131 cites W2042322631 @default.
• W2259685131 cites W2046033964 @default.
• W2259685131 cites W2060780410 @default.
• W2259685131 cites W2065265184 @default.
• W2259685131 cites W2068810452 @default.
• W2259685131 cites W2071314435 @default.
• W2259685131 cites W2071466655 @default.
• W2259685131 cites W2076724888 @default.
• W2259685131 cites W2079261398 @default.
• W2259685131 cites W2080811170 @default.
• W2259685131 cites W2095023595 @default.
• W2259685131 cites W2112687243 @default.
• W2259685131 cites W2118131023 @default.
• W2259685131 cites W2123731707 @default.
• W2259685131 cites W2125417060 @default.
• W2259685131 cites W2126716316 @default.
• W2259685131 cites W2136015516 @default.
• W2259685131 cites W2146316552 @default.
• W2259685131 cites W2152589822 @default.
• W2259685131 cites W2157101172 @default.
• W2259685131 cites W2163081670 @default.
• W2259685131 doi "https://doi.org/10.5194/acp-16-541-2016" @default.
• W2259685131 hasPublicationYear "2016" @default.
• W2259685131 type Work @default.
• W2259685131 sameAs 2259685131 @default.
• W2259685131 citedByCount "14" @default.
• W2259685131 countsByYear W22596851312016 @default.
• W2259685131 countsByYear W22596851312017 @default.
• W2259685131 countsByYear W22596851312018 @default.
• W2259685131 countsByYear W22596851312019 @default.
• W2259685131 countsByYear W22596851312020 @default.
• W2259685131 countsByYear W22596851312021 @default.
• W2259685131 countsByYear W22596851312023 @default.
• W2259685131 crossrefType "journal-article" @default.
• W2259685131 hasAuthorship W2259685131A5032017067 @default.
• W2259685131 hasAuthorship W2259685131A5045109869 @default.
• W2259685131 hasAuthorship W2259685131A5054274097 @default.
• W2259685131 hasBestOaLocation W22596851311 @default.
• W2259685131 hasConcept C109663097 @default.
• W2259685131 hasConcept C115852967 @default.
• W2259685131 hasConcept C121332964 @default.
• W2259685131 hasConcept C127313418 @default.
• W2259685131 hasConcept C140820882 @default.
• W2259685131 hasConcept C153294291 @default.
• W2259685131 hasConcept C157331469 @default.
• W2259685131 hasConcept C171420983 @default.
• W2259685131 hasConcept C18101618 @default.
• W2259685131 hasConcept C200114574 @default.
• W2259685131 hasConcept C39432304 @default.
• W2259685131 hasConcept C49204034 @default.
• W2259685131 hasConcept C53631411 @default.
• W2259685131 hasConcept C58024561 @default.
• W2259685131 hasConcept C62520636 @default.
• W2259685131 hasConcept C74902906 @default.
• W2259685131 hasConcept C9075549 @default.
• W2259685131 hasConcept C91586092 @default.
• W2259685131 hasConcept C97355855 @default.
• W2259685131 hasConceptScore W2259685131C109663097 @default.
• W2259685131 hasConceptScore W2259685131C115852967 @default.
• W2259685131 hasConceptScore W2259685131C121332964 @default.
• W2259685131 hasConceptScore W2259685131C127313418 @default.
• W2259685131 hasConceptScore W2259685131C140820882 @default.
• W2259685131 hasConceptScore W2259685131C153294291 @default.
• W2259685131 hasConceptScore W2259685131C157331469 @default.
• W2259685131 hasConceptScore W2259685131C171420983 @default.
• W2259685131 hasConceptScore W2259685131C18101618 @default.
• W2259685131 hasConceptScore W2259685131C200114574 @default.
• W2259685131 hasConceptScore W2259685131C39432304 @default.
• W2259685131 hasConceptScore W2259685131C49204034 @default.
• W2259685131 hasConceptScore W2259685131C53631411 @default.
• W2259685131 hasConceptScore W2259685131C58024561 @default.
• W2259685131 hasConceptScore W2259685131C62520636 @default.
• W2259685131 hasConceptScore W2259685131C74902906 @default.
• W2259685131 hasConceptScore W2259685131C9075549 @default.
• W2259685131 hasConceptScore W2259685131C91586092 @default.
• W2259685131 hasConceptScore W2259685131C97355855 @default.
• W2259685131 hasFunder F4320320879 @default.
• W2259685131 hasIssue "2" @default.
• W2259685131 hasLocation W22596851311 @default.
• W2259685131 hasLocation W22596851312 @default.

• next