Zobrazeno 1 - 10
of 1 463
pro vyhledávání: '"L. ACKERMANN"'
Publikováno v:
Geoscientific Model Development, Vol 17, Pp 3279-3301 (2024)
The explicit representation of cryospheric components in Earth system models has become more and more important over the last years. However, there are few advanced coupled Earth system models that employ interactive icebergs, and most iceberg model
Externí odkaz:
https://doaj.org/article/c53df362f72a4166b0f3f59e6c5e9d68
Autor:
T. Alinejadtabrizi, F. Lang, Y. Huang, L. Ackermann, M. Keywood, G. Ayers, P. Krummel, R. Humphries, A. G. Williams, S. T. Siems, M. Manton
Publikováno v:
npj Climate and Atmospheric Science, Vol 7, Iss 1, Pp 1-12 (2024)
Abstract Southern Ocean (SO) air is amongst the most pristine on Earth, particularly during winter. Historically, there has been a focus on biogenic sources as an explanation for the seasonal cycle in cloud condensation nuclei concentrations (N CCN).
Externí odkaz:
https://doaj.org/article/ad9fb95001d5467496b1e8208df49ec5
Publikováno v:
Atmospheric Chemistry and Physics, Vol 24, Pp 1451-1466 (2024)
Marine atmospheric boundary layer (MABL) clouds cover vast areas over the ocean and have important radiative effects on the Earth's climate system. These radiative effects are known to be sensitive to the local organization, or structure, of the meso
Externí odkaz:
https://doaj.org/article/85af9935a6fb4ae9b6228151dc5b8541
Publikováno v:
Atmospheric Measurement Techniques, Vol 17, Pp 407-422 (2024)
Large hail events are typically infrequent, with significant time gaps between occurrences at specific locations. However, when these events do happen, they can cause rapid and substantial economic losses within a matter of minutes. Therefore, it is
Externí odkaz:
https://doaj.org/article/a179b7f3a3674518a1991987c5f8a2b8
Publikováno v:
Atmospheric Chemistry and Physics, Vol 22, Pp 2135-2152 (2022)
Marine atmospheric boundary layer clouds cover vast areas of the Southern Ocean (SO), where they are commonly organized into mesoscale cellular convection (MCC). Using 3 years of Himawari-8 geostationary satellite observations, open and closed MCC st
Externí odkaz:
https://doaj.org/article/fdc6f3bcda8840e0898286d31eea2aaa
Autor:
B. Rappenglück, L. Ackermann, S. Alvarez, J. Golovko, M. Buhr, R. A. Field, J. Soltis, D. C. Montague, B. Hauze, S. Adamson, D. Risch, G. Wilkerson, D. Bush, T. Stoeckenius, C. Keslar
Publikováno v:
Atmospheric Chemistry and Physics, Vol 14, Iss 10, Pp 4909-4934 (2014)
During recent years, elevated ozone (O3) values have been observed repeatedly in the Upper Green River basin (UGRB), Wyoming, during wintertime. This paper presents an analysis of high ozone days in late winter 2011 (1 h average up to 166 ppbv – pa
Externí odkaz:
https://doaj.org/article/6dc3b455751d4263a0436bac8db95f57
Publikováno v:
Curationis, Vol 25, Iss 2, Pp 4-13 (2002)
In the effort to stem the HIV pandemic, the promotion of the correct and consistent use of condoms has to be a priority in the primary health care sector. This study, concentrating on the southern Free State, sought to identify obstacles to condom us
Externí odkaz:
https://doaj.org/article/47d4da92f62043018fe569c3fa4f8d1b
Autor:
Semi Zouiouich, Doratha A. Byrd, Xing Hua, Smriti Karwa, Yunhu Wan, Jianxin Shi, Gregory C. Humphrey, Gail L. Ackermann, Rob Knight, Christian C. Abnet, Emily Vogtmann, Rashmi Sinha
Publikováno v:
Cancer Epidemiology, Biomarkers & Prevention. 32:444-451
Background:In prospective cohorts, biological samples are generally stored over long periods before an adequate number of cases have accrued. We investigated the impact of sample storage at −80°C for 2 years on the stability of the V4 region of th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::588354dee854f4340fa121fa0a6871a5
https://doi.org/10.1158/1055-9965.epi-22-0883
https://doi.org/10.1158/1055-9965.epi-22-0883
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.