Titlebook: Climate Variability and Extremes during the Past 100 years; Stefan Brönnimann,Jürg Luterbacher,Urs Neu Book 2008 Springer Science+Business

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https://doi.org/10.1007/978-1-4684-8670-4r to construct a single atmospheric temperature data set from these measurements, data from a number of satellites must be combined, since each satellite operated only during a small part of the longer time period. If the combined data set is to be of sufficient quality to evaluate changes on the de

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https://doi.org/10.1007/978-3-642-97242-3 sea ice cover is reported during the late 1990s and 2000s both based on satellite observations of sea ice extent and model simulations of sea ice thickness. The observed and modeled changes are in qualitative agreement but model results imply higher rate of ice thickness decline compared to sea ice

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Sectional Curvature Comparison I,of greenhouse gases and aerosol in the atmosphere. Radiative energy reaching the ground is particularly important for mankind as it is a key determinant of the climate of our environments and strongly influences the thermal and hydrological conditions at the Earth surface. Recent evidence suggests t

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Sectional Curvature Comparison I,synoptic observations and from satellite data produced by the International Satellite Cloud Climatology Project. Substantial agreement exists between global mean time series of surface- and satellite-observed upper-level cloud cover, indicating that the reported variations in this cloud type are lik

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Sectional Curvature Comparison II,open one. While there is a microphysical link between an increase in aerosols and an increase in cloud albedo, a direct link to surface precipitation is less straight forward because it involves interactions between cloud microphysics and dynamics. Locally it has been suggested that in some instance

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Sectional Curvature Comparison I,ry. Facing recent climate changes, phenology has two major functions. Firstly, it reveals measurable impacts of climate change on nature, which at the same time clearly demonstrate global climate change in people’s backyards. Secondly, long-term phenological data allow the reconstruction of temperat

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