Zobrazeno 1 - 10
of 174
pro vyhledávání: '"T. Goren"'
Publikováno v:
Atmospheric Chemistry and Physics, Vol 23, Pp 9365-9383 (2023)
Marine cold-air outbreaks are important parts of the high-latitude climate system and are characterised by strong surface fluxes generated by the air–sea temperature gradient. These fluxes promote cloud formation, which can be identified in satelli
Externí odkaz:
https://doaj.org/article/b8d9fd8966e846d8805eee7ca4c5ba7b
Publikováno v:
Atmospheric Chemistry and Physics, Vol 22, Pp 3303-3319 (2022)
The evaluation of radiative forcing associated with aerosol–cloud interactions remains a significant source of uncertainty in future climate projections. The problem is confounded by the fact that aerosol particles influence clouds locally and that
Externí odkaz:
https://doaj.org/article/287a0122a4c745f79b483e3edc85af48
Autor:
M. W. Christensen, A. Gettelman, J. Cermak, G. Dagan, M. Diamond, A. Douglas, G. Feingold, F. Glassmeier, T. Goren, D. P. Grosvenor, E. Gryspeerdt, R. Kahn, Z. Li, P.-L. Ma, F. Malavelle, I. L. McCoy, D. T. McCoy, G. McFarquhar, J. Mülmenstädt, S. Pal, A. Possner, A. Povey, J. Quaas, D. Rosenfeld, A. Schmidt, R. Schrödner, A. Sorooshian, P. Stier, V. Toll, D. Watson-Parris, R. Wood, M. Yang, T. Yuan
Publikováno v:
Atmospheric Chemistry and Physics, Vol 22, Pp 641-674 (2022)
Aerosol–cloud interactions (ACIs) are considered to be the most uncertain driver of present-day radiative forcing due to human activities. The nonlinearity of cloud-state changes to aerosol perturbations make it challenging to attribute causality i
Externí odkaz:
https://doaj.org/article/b67802aa319b4f9ea1ad4a07bfa66e71
Publikováno v:
Atmospheric Chemistry and Physics, Vol 22, Pp 861-880 (2022)
Quantification of the radiative adjustment of marine low clouds to aerosol perturbations, regionally and globally, remains the largest source of uncertainty in assessing current and future climate. One of the important steps towards quantifying the r
Externí odkaz:
https://doaj.org/article/c85169815f994a94b23bba92668e906f
Publikováno v:
Atmospheric Chemistry and Physics, Vol 21, Pp 6093-6109 (2021)
The response of cloud processes to an aerosol perturbation is one of the largest uncertainties in the anthropogenic forcing of the climate. It occurs at a variety of timescales, from the near-instantaneous Twomey effect to the longer timescales requi
Externí odkaz:
https://doaj.org/article/872cc88086844eab8f6b8b2f9c91d359
Autor:
E. Gryspeerdt, T. Goren, O. Sourdeval, J. Quaas, J. Mülmenstädt, S. Dipu, C. Unglaub, A. Gettelman, M. Christensen
Publikováno v:
Atmospheric Chemistry and Physics, Vol 19, Pp 5331-5347 (2019)
The impact of aerosols on cloud properties is one of the largest uncertainties in the anthropogenic radiative forcing of the climate. Significant progress has been made in constraining this forcing using observations, but uncertainty remains, particu
Externí odkaz:
https://doaj.org/article/4ae9228f037d423089104db166d9493b
Autor:
O. Sourdeval, E. Gryspeerdt, M. Krämer, T. Goren, J. Delanoë, A. Afchine, F. Hemmer, J. Quaas
Publikováno v:
Atmospheric Chemistry and Physics, Vol 18, Pp 14327-14350 (2018)
The number concentration of cloud particles is a key quantity for understanding aerosol–cloud interactions and describing clouds in climate and numerical weather prediction models. In contrast with recent advances for liquid clouds, few observat
Externí odkaz:
https://doaj.org/article/1cd3c6c777ed496db2bb659bb63e6725
Publikováno v:
Atmospheric Chemistry and Physics, Vol 18, Pp 6157-6169 (2018)
Cirrus clouds play an important role in determining the radiation budget of the earth, but many of their properties remain uncertain, particularly their response to aerosol variations and to warming. Part of the reason for this uncertainty is the
Externí odkaz:
https://doaj.org/article/e768adb132bc48558cefed7af483a873
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Akademický článek
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