Zobrazeno 1 - 10
of 192
pro vyhledávání: '"J, Sedlar"'
Publikováno v:
Atmospheric Chemistry and Physics, Vol 22, Pp 8973-8988 (2022)
Mixed-phase clouds are ubiquitous in the Arctic. These clouds can persist for days and dissipate in a matter of hours. It is sometimes unknown what causes this sudden dissipation, but aerosol–cloud interactions may be involved. Arctic aerosol conce
Externí odkaz:
https://doaj.org/article/670b572225a94740b4ed3e95a6a27bac
Autor:
J. B. Duncan Jr., L. Bianco, B. Adler, T. Bell, I. V. Djalalova, L. Riihimaki, J. Sedlar, E. N. Smith, D. D. Turner, T. J. Wagner, J. M. Wilczak
Publikováno v:
Atmospheric Measurement Techniques, Vol 15, Pp 2479-2502 (2022)
During the Chequamegon Heterogeneous Ecosystem Energy-balance Study Enabled by a High-density Extensive Array of Detectors 2019 (CHEESEHEAD19) field campaign, held in the summer of 2019 in northern Wisconsin, USA, active and passive ground-based remo
Externí odkaz:
https://doaj.org/article/857c472253804f9e89fa384326af9912
Publikováno v:
Atmospheric Chemistry and Physics, Vol 21, Pp 4149-4167 (2021)
Clear-sky periods across the high latitudes have profound impacts on the surface energy budget and lower atmospheric stratification; however an understanding of the atmospheric processes leading to low-level cloud dissipation and formation events is
Externí odkaz:
https://doaj.org/article/9721410f04874f51bd6c0b8e7160ef7b
Publikováno v:
Atmospheric Chemistry and Physics, Vol 17, Pp 6693-6704 (2017)
The Arctic climate is changing; temperature changes in the Arctic are greater than at midlatitudes, and changing atmospheric conditions influence Arctic mixed-phase clouds, which are important for the Arctic surface energy budget. These low-level
Externí odkaz:
https://doaj.org/article/61144130d8e74c5ca065c227b1101043
Autor:
K.-G. Karlsson, K. Anttila, J. Trentmann, M. Stengel, J. Fokke Meirink, A. Devasthale, T. Hanschmann, S. Kothe, E. Jääskeläinen, J. Sedlar, N. Benas, G.-J. van Zadelhoff, C. Schlundt, D. Stein, S. Finkensieper, N. Håkansson, R. Hollmann
Publikováno v:
Atmospheric Chemistry and Physics, Vol 17, Iss 9, Pp 5809-5828 (2017)
The second edition of the satellite-derived climate data record CLARA (The CM SAF Cloud, Albedo And Surface Radiation dataset from AVHRR data – second edition denoted as CLARA-A2) is described. The data record covers the 34-year period from 1982 un
Externí odkaz:
https://doaj.org/article/355536fdff114353a82fb5ad467a5fe6
Akademický článek
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Akademický článek
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Publikováno v:
Atmospheric Chemistry and Physics, Vol 14, Iss 22, Pp 12573-12592 (2014)
The vertical structure of Arctic low-level clouds and Arctic boundary layer is studied, using observations from ASCOS (Arctic Summer Cloud Ocean Study), in the central Arctic, in late summer 2008. Two general types of cloud structures are examined: t
Externí odkaz:
https://doaj.org/article/8f0004ddb4e642cd9f3a7a7b7e364673
Autor:
T. Vihma, R. Pirazzini, I. Fer, I. A. Renfrew, J. Sedlar, M. Tjernström, C. Lüpkes, T. Nygård, D. Notz, J. Weiss, D. Marsan, B. Cheng, G. Birnbaum, S. Gerland, D. Chechin, J. C. Gascard
Publikováno v:
Atmospheric Chemistry and Physics, Vol 14, Iss 17, Pp 9403-9450 (2014)
The Arctic climate system includes numerous highly interactive small-scale physical processes in the atmosphere, sea ice, and ocean. During and since the International Polar Year 2007–2009, significant advances have been made in understanding these
Externí odkaz:
https://doaj.org/article/0685dba2ffeb40a2b3029b2fbf45ba18
Autor:
J. Sedlar, M. D. Shupe
Publikováno v:
Atmospheric Chemistry and Physics, Vol 14, Iss 7, Pp 3461-3478 (2014)
Over the Arctic Ocean, little is known on cloud-generated buoyant overturning vertical motions within mixed-phase stratocumulus clouds. Characteristics of such motions are important for understanding the diabatic processes associated with the vertica
Externí odkaz:
https://doaj.org/article/ec912604ee224046a3464803aaa62b67