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First 711 results for ” K Thomas”

1. The heavy precipitation event of May-June 2013 in the upper Danube and Elbe basins

   An observation-based analysis and large simulation ensembles show no evidence that climate change...

   N Schaller, FEL Otto, GJ van Oldenborgh, NR Massey, S Sparrow, MR Allan | Status: published | Journal: Bull. Amer. Meteor. Soc. | Volume: 95 | Year: 2014 | First page: S69 | Last page: S72

   Publication

2. What can 14CO measurements tell us about OH?

   The possible use of 14CO measurements to constrain hydroxyl radical (OH) concentrations in the at...

   MC Krol, JF Meirink, P Bergamaschi, JE Mak, D Lowe, P Joeckel, S Houweling, T Roeckmann | Status: published | Journal: Atm. Chem. Phys. | Volume: 8 | Year: 2008 | First page: 5033 | Last page: 5044 | doi: direct.sref.org/1680-7324/acp/2008-8-5033

   Publication

3. Towards an integrated seasonal forecasting system for South America

   This study proposes an integrated seasonal forecasting system for producing improved and well-cal...

   CAS Coelho, DB Stephenson, MA Balmaseda, FJ Doblas-Reyes, GJ van Oldenborgh | Status: published | Journal: J. Climate | Volume: 19 | Year: 2006 | First page: 3704 | Last page: 3721 | doi: 10.1175/JCLI3801.1

   Publication

4. Interannual variability and trend of CH4 lifetime as a measure for OH changes in the 1979-1993 time period
   F Dentener, W Peters, M Krol, M van Weele, P Bergamaschi, J Lelieveld | Status: published | Journal: J. Geophys. Res. | Volume: 108 | Year: 2003 | First page: 4442 | doi: 10.1029/2002JD002916

   Publication

5. A Bayesian approach for multi-model downscaling: Seasonal forecasting of regional rainfall and river flows in South America

   This study addresses three issues: spatial downscaling, calibration, and combination of seasonal ...

   CAS Coelho, DB Stephenson, FJ Doblas-Reyes, M Balmaseda, GJ van Oldenborgh | Status: published | Journal: Meteorological Applications (Royal Met. Society) | Volume: 13 | Year: 2006 | First page: 73 | Last page: 82 | doi: 10.1017/S1350482705002045

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