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First 5200 results for ” Bart van den Hurk and Geert Lenderink”

1. Divergent trajectories of Antarctic surface melt under two twenty-first-century climate scenarios

   Ice shelves modulate Antarctic contributions to sea-level rise1 and thereby represent a critical,...

   LD Trusel, KE Frey, SB Dias, KB Karnauskas, P Kuipers Munneke, E van Meijgaard, MR van den Broeke | Status: published | Journal: Nature Geoscience | Volume: 8 | Year: 2015 | First page: 927 | Last page: 932 | doi: 10.1038/NGEO2563

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2. Attribution of Wintertime Anticyclonic Stagnation Contributing to Air Pollution in Western Europe

   Climate simulations suggest a potential increase in frequency of stagnant wintertime conditions t...

   R Vautard, A Colette, E van Meijgaard, F Meleux, GJ van Oldenborgh, FEL Otto, I Tobin, P Yiou | Status: published | Journal: Bull. Amer. Meteor. Soc. | Volume: 99 | Year: 2018 | First page: S70 | Last page: S75 | doi: 10.1175/BAMS-D-17-0113.1

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3. The generation of EarthCARE L1 test data sets using atmospheric model data sets

   The Earth Cloud, Aerosol and Radiation Explorer mission (EarthCARE) is a multi-instrument cloud–a...

   David P Donovan, Pavlos Kollias, Almudena Velázquez Blázquez, Gerd-Jan van Zadelhoff | Journal: Atmospheric Measurement Techniques | Volume: 16 | Year: 2023 | First page: 5327 | Last page: 5356 | doi: 10.5194/amt-16-5327-2023

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4. Weather, seasonal and decadal forecasting: synthesis of past OSE/OSSE activities and OSE/OSSE plans

   The planned experiments for the work package on seasonal to decadal forecasting within E-AIMS are...

   RR King, M Martin, A Sterl | Year: 2013

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5. Aerosol Influence on Polarization and Intensity in Near-Infrared O2 and CO2 Absorption Bands Observed from Space

   We study the intensity and degree of linear polarization of reflected solar radiation at the top ...

   E Boesche, P Stammes, R Bennartz | Status: published | Journal: J. Quant. Spectros. Rad. Transf. | Volume: 110 | Year: 2009 | First page: 223 | Last page: 239 | doi: 10.1016/j.jqsrt.2008.09.019

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