Zobrazeno 1 - 10
of 41
pro vyhledávání: '"C. Dione"'
Autor:
C. Dione, M. Haeffelin, F. Burnet, C. Lac, G. Canut, J. Delanoë, J.-C. Dupont, S. Jorquera, P. Martinet, J.-F. Ribaud, F. Toledo
Publikováno v:
Atmospheric Chemistry and Physics, Vol 23, Pp 15711-15731 (2023)
In this study, we use a synergy of in situ and remote sensing measurements collected during the SOuthwest FOGs 3D experiment for processes study (SOFOG3D) field campaign in autumn and winter 2019–2020 to analyse the thermodynamic and turbulent proc
Externí odkaz:
https://doaj.org/article/f32cd0cf4f6f4a49a89199633b3afbba
Autor:
A. Deroubaix, L. Menut, C. Flamant, P. Knippertz, A. H. Fink, A. Batenburg, J. Brito, C. Denjean, C. Dione, R. Dupuy, V. Hahn, N. Kalthoff, F. Lohou, A. Schwarzenboeck, G. Siour, P. Tuccella, C. Voigt
Publikováno v:
Atmospheric Chemistry and Physics, Vol 22, Pp 3251-3273 (2022)
During the West African summer monsoon, pollutants emitted in urbanized coastal areas modify cloud cover and precipitation patterns. The Dynamics-Aerosol-Chemistry-Cloud Interactions in West Africa (DACCIWA) field campaign provided numerous aircraft-
Externí odkaz:
https://doaj.org/article/8acfb3f58ff3475d92d3645d60414988
Autor:
M. Zouzoua, F. Lohou, P. Assamoi, M. Lothon, V. Yoboue, C. Dione, N. Kalthoff, B. Adler, K. Babić, X. Pedruzo-Bagazgoitia, S. Derrien
Publikováno v:
Atmospheric Chemistry and Physics, Vol 21, Pp 2027-2051 (2021)
Within the framework of the DACCIWA (Dynamics–Aerosol–Chemistry–Cloud Interactions in West Africa) project and based on a field experiment conducted in June and July 2016, we analyze the daytime breakup of continental low-level stratiform cloud
Externí odkaz:
https://doaj.org/article/7120ef809bb742e7bdc6dc54d5f1672a
Autor:
B. Altstädter, K. Deetz, B. Vogel, K. Babić, C. Dione, F. Pacifico, C. Jambert, F. Ebus, K. Bärfuss, F. Pätzold, A. Lampert, B. Adler, N. Kalthoff, F. Lohou
Publikováno v:
Atmospheric Chemistry and Physics, Vol 20, Pp 7911-7928 (2020)
This study underlines the important role of the transported black carbon (BC) mass concentration in the West African monsoon (WAM) area. BC was measured with a micro-aethalometer integrated in the payload bay of the unmanned research aircraft ALADINA
Externí odkaz:
https://doaj.org/article/aac8746c55544f0098bb56dadb46ed8e
Autor:
X. Pedruzo-Bagazgoitia, S. R. de Roode, B. Adler, K. Babić, C. Dione, N. Kalthoff, F. Lohou, M. Lothon, J. Vilà-Guerau de Arellano
Publikováno v:
Atmospheric Chemistry and Physics, Vol 20, Pp 2735-2754 (2020)
The misrepresentation of the diurnal cycle of boundary layer clouds by large-scale models strongly impacts the modeled regional energy balance in southern West Africa. In particular, recognizing the processes involved in the maintenance and transitio
Externí odkaz:
https://doaj.org/article/e5bb9070c5a34bda8740efdd66b4b083
Autor:
F. Lohou, N. Kalthoff, B. Adler, K. Babić, C. Dione, M. Lothon, X. Pedruzo-Bagazgoitia, M. Zouzoua
Publikováno v:
Atmospheric Chemistry and Physics, Vol 20, Pp 2263-2275 (2020)
The DACCIWA (Dynamics Aerosol Chemistry Cloud Interactions in West Africa) project and the associated ground-based field experiment, which took place during summer 2016, provided a comprehensive dataset on the low-level stratiform clouds (LLSCs), whi
Externí odkaz:
https://doaj.org/article/297b9cd0ff774cd1ad97a858e01ec538
Publikováno v:
Atmospheric Chemistry and Physics, Vol 19, Pp 13489-13506 (2019)
Nocturnal low-level stratus clouds (LLCs) are frequently observed in the atmospheric boundary layer (ABL) over southern West Africa (SWA) during the summer monsoon season. Considering the effect these clouds have on the surface energy and radiation b
Externí odkaz:
https://doaj.org/article/839c789c35084c92a161689c3ac9452d
Low-level stratiform clouds and dynamical features observed within the southern West African monsoon
Autor:
C. Dione, F. Lohou, M. Lothon, B. Adler, K. Babić, N. Kalthoff, X. Pedruzo-Bagazgoitia, Y. Bezombes, O. Gabella
Publikováno v:
Atmospheric Chemistry and Physics, Vol 19, Pp 8979-8997 (2019)
During the boreal summer, the monsoon season that takes place in West Africa is accompanied by low stratus clouds over land that stretch from the Guinean coast several hundred kilometers inland. Numerical climate and weather models need finer descrip
Externí odkaz:
https://doaj.org/article/6ec51610111543a18a0b347b4ca85df9
Autor:
S. L. Haslett, J. W. Taylor, K. Deetz, B. Vogel, K. Babić, N. Kalthoff, A. Wieser, C. Dione, F. Lohou, J. Brito, R. Dupuy, A. Schwarzenboeck, P. Zieger, H. Coe
Publikováno v:
Atmospheric Chemistry and Physics, Vol 19, Pp 1505-1520 (2019)
Water in the atmosphere can exist in the solid, liquid or gas phase. At high humidities, if the aerosol population remains constant, more water vapour will condense onto the particles and cause them to swell, sometimes up to several times their origi
Externí odkaz:
https://doaj.org/article/cc4754c01bb04f56a82ed13715293a9d
Autor:
B. Adler, K. Babić, N. Kalthoff, F. Lohou, M. Lothon, C. Dione, X. Pedruzo-Bagazgoitia, H. Andersen
Publikováno v:
Atmospheric Chemistry and Physics, Vol 19, Pp 663-681 (2019)
During the West African summer monsoon season, extended nocturnal stratiform low-level clouds (LLCs) frequently form in the atmospheric boundary layer over southern West Africa and persist long into the following day affecting the regional climate. A
Externí odkaz:
https://doaj.org/article/7648944e37554656891f59febeb1e217