Surface layer

Results: 805



#Item
1Modeling the Atmospheric Boundary Layer Wind Response to Mesoscale Sea Surface Temperature Perturbations Natalie Perlin1, Simon P. de Szoeke2, Dudley B. Chelton2, Roger M. Samelson2, Eric D. Skyllingstad2, and Larry W. O

Modeling the Atmospheric Boundary Layer Wind Response to Mesoscale Sea Surface Temperature Perturbations Natalie Perlin1, Simon P. de Szoeke2, Dudley B. Chelton2, Roger M. Samelson2, Eric D. Skyllingstad2, and Larry W. O

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Source URL: www-poa.coas.oregonstate.edu

- Date: 2014-08-05 19:45:12
    2Oil that is spilled in the ocean floats on the surface of the water. It spreads out quickly to form a thin layer called an oil slick. As the spreading continues, the layer becomes thinner and thinner. It finally becomes

    Oil that is spilled in the ocean floats on the surface of the water. It spreads out quickly to form a thin layer called an oil slick. As the spreading continues, the layer becomes thinner and thinner. It finally becomes

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    Source URL: www.lamotte.com

    - Date: 2013-07-31 10:21:08
      3Surface fluxes, temperatures and boundary layer evolution at the building greyzone in London Supervisors: Prof Sue Grimmond (University of Reading), Dr Sylvia Bohnenstengel (Met Office@ Reading), Dr Humphrey Lean (Met Of

      Surface fluxes, temperatures and boundary layer evolution at the building greyzone in London Supervisors: Prof Sue Grimmond (University of Reading), Dr Sylvia Bohnenstengel (Met Office@ Reading), Dr Humphrey Lean (Met Of

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      Source URL: urban-climate.org

      - Date: 2016-06-10 14:06:37
        4Specification for Ocean Surface Vector Stress (OSVS) Preamble/Introduction. Ocean surface vector stress (OSVS) is also the drag at the bottom of the atmosphere and the dynamical forcing at the top of the ocean. OSVS is t

        Specification for Ocean Surface Vector Stress (OSVS) Preamble/Introduction. Ocean surface vector stress (OSVS) is also the drag at the bottom of the atmosphere and the dynamical forcing at the top of the ocean. OSVS is t

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        Source URL: ioc-goos-oopc.org

        Language: English - Date: 2016-02-25 08:57:46
        5KIMBERLITES Kimberlite is an ultrabasic olivine-rich igneous rock called peridotite. Peridotites occur at great depths in the earth in a layer called the mantlemiles below the surface). At this depth the combi

        KIMBERLITES Kimberlite is an ultrabasic olivine-rich igneous rock called peridotite. Peridotites occur at great depths in the earth in a layer called the mantlemiles below the surface). At this depth the combi

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        Source URL: www.uky.edu

        Language: English - Date: 2016-04-04 14:15:46
        6Chapter 5 Surface Waves Post-Critical Planar SH waves In the last chapter we discussed how to solve the problem of a planar SH-wave incident from a half space onto the bottom of a layer welded on that half space. In this

        Chapter 5 Surface Waves Post-Critical Planar SH waves In the last chapter we discussed how to solve the problem of a planar SH-wave incident from a half space onto the bottom of a layer welded on that half space. In this

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        Source URL: www.its.caltech.edu

        Language: English - Date: 2005-07-07 19:13:16
        7Forum geografic. Studii și cercetări de geografie și protecția mediului Volume XIV, Issue 2 (December 2015), pphttp://dx.doi.orgfg091.d Near surface thermal characteristics of

        Forum geografic. Studii și cercetări de geografie și protecția mediului Volume XIV, Issue 2 (December 2015), pphttp://dx.doi.orgfg091.d Near surface thermal characteristics of

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        Source URL: forumgeografic.ro

        Language: English - Date: 2016-02-06 15:31:51
        8AXBT Observation of Upper-Ocean Temperature During CalWater2 Sue Chen1, Peter Black2, James Doyle1 1Naval INTRODUCTION

        AXBT Observation of Upper-Ocean Temperature During CalWater2 Sue Chen1, Peter Black2, James Doyle1 1Naval INTRODUCTION

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        Source URL: www.nanoos.org

        Language: English - Date: 2016-03-10 13:52:37
        9

        PDF Document

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        Source URL: www.dpac.dpri.kyoto-u.ac.jp

        Language: English - Date: 2014-04-21 04:05:32
        10HWRF Surface Layer Evaluations Eric W. Uhlhorn Joseph J. Cione NOAA/AOML/HRD Special thanks to HRD HWRF Model Team:

        HWRF Surface Layer Evaluations Eric W. Uhlhorn Joseph J. Cione NOAA/AOML/HRD Special thanks to HRD HWRF Model Team:

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        Source URL: www.hfip.org

        Language: English - Date: 2012-10-26 18:10:09