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First 537 results for ” A Kokhanosky”

1. Tropospheric ozone determined from Aura OMI and MLS: Evaluation of measurements and comparison with the Global Modeling Initiative’s Chemical Transport Model

   Ozone measurements from the OMI and MLS instruments onboard the Aura satellite are used for deriv...

   JR Ziemke, S Chandra, BN Duncan, L Froidevaux, PK Bhartia, PF Levelt, JW Waters | Status: published | Journal: J. Geophys. Res. | Volume: 111 | Year: 2006 | First page: D19303 | doi: 10.1029/2006JD007089

   Publication

2. Estimated changes in flood quantiles of the river Meuse from resampling of regional climate model output

   Precipitation and temperature data from three regional climate model (RCM) experiments were used ...

   R Leander, TA Buishand, BJJM van den Hurk, MJM de Wit | Status: published | Journal: J. Hydrol. | Volume: 351 | Year: 2008 | First page: 331 | Last page: 343 | doi: 10.1016/j.jhydrol.2007.12.020

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3. Intra-seasonal variability in tropospheric ozone and water vapor in the tropics
   JR Ziemke, S Chandra, MR Schoeberl, L Froidevaux, WG Read, PF Levelt, PK Bhartia | Status: published | Journal: Geophys. Res. Lett. | Volume: 34 | Year: 2007 | First page: L17804 | doi: 10.1029/2007GL030965

   Publication

4. A synthesis of hourly and daily precipitation extremes in different climatic regions
   R Barbero, HJ Fowler, S Blenkinsop, S Westra, V Moron, E Lewis, S Chan, G Lenderink, Et al. | Status: published | Journal: Weather and Climate Extremes | Volume: 26 | Year: 2019 | First page: 100219 | doi: https://doi.org/10.1016/j.wace.2019.100219

   Publication

5. The influence of aggregation and statistical post‐processing on the subseasonal predictability of European temperatures

   The succession of European surface weather patterns has limited predictability because disturbanc...

   C van Straaten, K Whan, D Coumou, B van den Hurk, M Schmeits | Status: published | Journal: Quart. J. Royal Meteor. Soc. | Volume: 146 | Year: 2020 | First page: 2654 | Last page: 2670 | doi: 10.1002/qj.3810

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