Zobrazeno 1 - 10
of 195
pro vyhledávání: '"Robert J. Charlson"'
Publikováno v:
Tellus: Series B, Chemical and Physical Meteorology, Vol 67, Iss 0, Pp 1-9 (2015)
Earth's albedo is the primary determinant of the amount of energy absorbed by the Earth–atmosphere system. It is a function of the fractional cloud cover and the cloudy- and clear-sky albedos, and thereby of the aerosol loading of the atmosphere. H
Externí odkaz:
https://doaj.org/article/b9be16c474f04ddbbd10e4cb30338248
Autor:
Jost Heintzenberg, Robert J. Charlson
Experts consider the many roles that clouds play in the the changing climate—one of the least understood and most puzzling aspects of atmospheric science.More than half the globe is covered by visible clouds. Clouds control major parts of the Earth
Publikováno v:
Journal of Climate. 30:4131-4147
The hemispheric symmetry of albedo and its contributing factors in satellite observations and global climate models is evaluated. The analysis is performed on the annual mean time scale, on which a bimodality in the joint distribution of albedo and c
Publikováno v:
Geophysical Research Letters. 42:9571-9578
We study the relation between monthly mean albedo and cloud fraction over ocean,60∘S–60∘N. Satellite obser vations indicate that these clouds all fall on the same near-exponential curve,with a mono ...
Publikováno v:
Tellus: Series B, Chemical and Physical Meteorology, Vol 67, Iss 0, Pp 1-9 (2015)
Tellus B; Vol 67 (2015)
Tellus B; Vol 67 (2015)
Earth’s albedo is the primary determinant of the amount of energy absorbed by the Earth–atmosphere system. It is a function of the fractional cloud cover and the cloudy- and clear-sky albedos, and thereby of the aerosol loading of the atmosphere.
Autor:
Matthias Tesche, Paul Zieger, Robert J. Charlson, Hans-Christen Hansson, Narges Rastak, Peter Tunved, Paul Glantz
Publikováno v:
Atmospheric Chemistry and Physics, Vol 14, Iss 15, Pp 7869-7882 (2014)
Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics
In this study we investigate to what degree it is possible to reconcile continuously recorded particle light extinction coefficients derived from dry in situ measurements at Zeppelin station (78.92° N, 11.85° E; 475 m above sea level), Ny-Ålesund,
Publikováno v:
Journal of Climate. 25:2200-2204
In response to our article, Why Hasnt Earth Warmed as Much as Expected? (2010), Knutti and Plattner (2012) wrote a rebuttal. The term climate sensitivity is usually defined as the change in global mean surface temperature that is produced by a specif
Publikováno v:
Journal of Applied Meteorology and Climatology. 50:2139-2148
Planetary albedo—the reflectivity for solar radiation—is of singular importance in determining the amount of solar energy taken in by the Earth–atmosphere system. Modeling albedo, and specifically cloud albedo, correctly is crucial for realisti
Autor:
Lamont R. Poole, Robert J. Charlson, Mark A. Vaughan, Qiang Fu, Bruce A. Wielicki, Peter R. Colarco, Pierre H. Flamant, Jacques Pelon, Chieko Kittaka, Chip Trepte, H. Le Treut, Gérard Mégie, M. P. McCormick, James A. Coakley, Steven A. Ackerman, Raymond M. Hoff, David M. Winker, Kathleen A. Powell, T. L. Kubar
Publikováno v:
Bulletin of the American Meteorological Society. 91:1211-1230
Aerosols and clouds have important effects on Earth's climate through their effects on the radiation budget and the cycling of water between the atmosphere and Earth's surface. Limitations in our understanding of the global distribution and propertie
Publikováno v:
Journal of Climate. 23:2453-2464
The observed increase in global mean surface temperature (GMST) over the industrial era is less than 40% of that expected from observed increases in long-lived greenhouse gases together with the best-estimate equilibrium climate sensitivity given by