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The effect of temporal variations in the surface mass balance and temperature-inversion strength on the interpretation of ice-core signals
The proxy for temperature (delta-signal) in ice cores is stored in the snow/ice during precipitat...
NPM van Lipzig, E van Meijgaard, J Oerlemans | Status: published | Journal: Journal of Glaciology | Volume: 48 | Year: 2002 | First page: 611 | Last page: 621
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Oscillations in Neutral Winds Observed by GOCE
This study explores intra‐annual oscillations (IAOs) in upper thermospheric winds using GOCE cros...
MS Dhadly, JT Emmert, M Jones, EN Doornbos, KA Zawdie, DP Drob, M Conde | Status: published | Journal: Geophys. Res. Lett. | Volume: 47 | Year: 2020 | doi: 10.1029/2020GL089339
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Is the intensification of precipitation extremes with global warming better detected at hourly than daily resolutions?
Although it has been documented that daily precipitation extremes are increasing worldwide, faste...
Barbero, Fowler, G Lenderink, G Blenkinsop | Status: published | Journal: Geophys. Res. Lett. | Volume: 44 | Year: 2017 | First page: 974 | Last page: 983 | doi: 10.1002/2016GL071917
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Cabauw meteorological data tapes 1973-1984 : description of instrumentation and data processing for the continuous measurements
Five tapes have been compiled, each containing half-hourly averages of the continuous measurement...
H.R.A. Wessels | Year: 1984 | Pages: 29
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Antarctic Ozone Hole [in ”State of the Climate in 2019”]
[from the full abstract] Above Earth’s surface, the annual lower troposphere temperature was thir...
A.T.J. de Laat | Journal: Bulletin of the American Meteorological Society | Volume: Volume 101: Issue 8 | Year: 2019 | First page: S1 | Last page: S429 | doi: 10.1175/2020BAMSStateoftheClimate.1
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