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First 1638 results for ” Engwell Samantha”

1. What controls the vertical distribution of aerosol? Relationships between process sensitivity in HadGEM3–UKCA and inter-model variation from AeroCom Phase II

   The vertical profile of aerosol is important for its radiative effects, but weakly constrained by...

   Z Kipling, P Stier, CE Johnson, GW Mann, N Bellouin, SE Bauer, T Bergman, M Chin, T Diehl, SJ Ghan, T Iversen, A Kirkevåg, H Kokkola, X Liu, G Luo, T van Noije, KJ Pringle, K von Salzen, M Schulz, Ø Seland, RB Skeie, T Takemura, K Tsigaridis, K Zhang | Status: published | Journal: Atmos. Chem. Phys. | Volume: 16 | Year: 2016 | First page: 2221 | Last page: 2241 | doi: 10.5194/acp-16-2221-2016

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2. Passive probing of the sound fixing and ranging channel with hydro-acoustic observations from ridge earthquakes

   The International Monitoring System includes a hydro-acoustic part to verify the Comprehensive Nu...

   LG Evers, M Snellen | Status: published | Journal: J.A.S.A. | Volume: 137 | Year: 2015 | First page: 2124 | doi: 10.1121/1.4916267

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3. Towards a standard procedure for validation of satellite-derived cloud liquid water path: a study with SEVIRI data

   Differences between satellite-derived and ground-based values of cloud liquid water path (LWPsat ...

   W Greuell, RA Roebeling | Status: published | Journal: J. Appl. Meteor. | Volume: 48 | Year: 2009 | First page: 1575 | Last page: 1590 | doi: 10.1175/2009JAMC2112.1

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4. A probabilistic approach for SeaWinds data assimilation
   M Portabella, A Stoffelen | Status: published | Journal: Quart. J. Royal Meteor. Soc. | Volume: 130 | Year: 2004 | First page: 127 | Last page: 159 | doi: 10.1256/qj.02.205

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5. A comparison of KNMI Quality Control and JPL Rain Flag for SeaWinds

   In the past few years, scatterometer winds have been successfully assimilated in weather analysis...

   M Portabella, A Stoffelen | Status: published | Journal: Canadian Journal of Remote Sensing | Volume: 28 | Year: 2002 | First page: 424 | Last page: 430 | doi: 10.5589/m02-040

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