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First 1037 results for ” R García Herrera”

  1. Drought and ecosystem carbon cycling

    Drought as an intermittent disturbance of the water cycle interacts with the carbon cycle differe...

    MK van der Molen, and coauthors, including, BJJM van den Hurk | Status: accepted | Journal: Agric. and Forest Met. | Year: 2011 | doi: 10.1016/j.agrformet.2011.01.018

    Publication

  2. How much could be gained from ocean-data assimilation if ENSO were a simple stochastic oscillator?

    Assimilation of sub-surface ocean data is one of the factors that have contributed to the increas...

    G Burgers | Conference: Third WMO international symposium on assimilation | Organisation: WMO (Geneva 2000) | Place: Quebec City | First page: 0 | Last page: 0

    Publication

  3. Applications of continuation methods in physical oceanography

    In this paper, continuation methods are used to study fundamental problems in physical oceanograp...

    CA Katsman, HA Dijkstra, MJ Schmeits | Conference: Continuation methods in Fluid Dynamics. ERCOFTAC/ | Organisation: Notes on Numerical Fluid mecha | First page: 155 | Last page: 166

    Publication

  4. 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

    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

    Publication