Upper atmospheric gravity wave details revealed in nightglow satellite imagery
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00020699%3A_____%2F15%3A%230000857" target="_blank" >RIV/00020699:_____/15:#0000857 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.1073/pnas.1508084112" target="_blank" >http://dx.doi.org/10.1073/pnas.1508084112</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1073/pnas.1508084112" target="_blank" >10.1073/pnas.1508084112</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Upper atmospheric gravity wave details revealed in nightglow satellite imagery
Popis výsledku v původním jazyce
Gravity waves (disturbances to the density structure of the atmosphere whose restoring forces are gravity and buoyancy) comprise the principal form of energy exchange between the lower and upper atmosphere. Wave breaking drives the mean upper atmosphericcirculation, determining boundary conditions to stratospheric processes, which in turn influence tropospheric weather and climate patterns on various spatial and temporal scales. Despite their recognized importance, very little is known about upper-level gravity wave characteristics. The knowledge gap is mainly due to lack of global, high-resolution observations from currently available satellite observing systems. Consequently, representations ofwave-related processes in global models are crude, highly parameterized, and poorly constrained, limiting the description of various processes influenced by them. Here we highlight, through a series of examples, the unanticipated ability of the Day/Night Band (DNB) on the NOAA/NASA Suomi Natio
Název v anglickém jazyce
Upper atmospheric gravity wave details revealed in nightglow satellite imagery
Popis výsledku anglicky
Gravity waves (disturbances to the density structure of the atmosphere whose restoring forces are gravity and buoyancy) comprise the principal form of energy exchange between the lower and upper atmosphere. Wave breaking drives the mean upper atmosphericcirculation, determining boundary conditions to stratospheric processes, which in turn influence tropospheric weather and climate patterns on various spatial and temporal scales. Despite their recognized importance, very little is known about upper-level gravity wave characteristics. The knowledge gap is mainly due to lack of global, high-resolution observations from currently available satellite observing systems. Consequently, representations ofwave-related processes in global models are crude, highly parameterized, and poorly constrained, limiting the description of various processes influenced by them. Here we highlight, through a series of examples, the unanticipated ability of the Day/Night Band (DNB) on the NOAA/NASA Suomi Natio
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DG - Vědy o atmosféře, meteorologie
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
V - Vyzkumna aktivita podporovana z jinych verejnych zdroju
Ostatní
Rok uplatnění
2015
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
PNAS
ISSN
0027-8424
e-ISSN
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Svazek periodika
112
Číslo periodika v rámci svazku
49
Stát vydavatele periodika
US - Spojené státy americké
Počet stran výsledku
8
Strana od-do
"E6728?E6735"
Kód UT WoS článku
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EID výsledku v databázi Scopus
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