Changeset 186 for trunk/adm


Ignore:
Timestamp:
04/12/12 15:02:31 (12 years ago)
Author:
pinsard
Message:

published paper ref. in doc

Location:
trunk/adm/website
Files:
7 edited

Legend:

Unmodified
Added
Removed
  • trunk/adm/website/Readme.rst

    r185 r186  
    88----------------------------- 
    99 
    10 The TropFlux project aims at providing daily, timely, accurate air-sea heat and momentum flux data for the entire 30°N-30°S region.  Wind stresses and the four components of net surface heat flux are currently available for the entire 1979 to eptember 2011 period. We are currently working on a regular (~monthly) update of the TropFlux product until 3-4 months behind realtime, which should be available in 2012. 
     10The TropFlux project aims at providing daily, timely, accurate air-sea heat and momentum flux data for the entire 30°N-30°S region.  Wind stresses and the four components of net surface heat flux are currently available for the entire 1979 to september 2011 period. We are currently working on a regular (~monthly) update of the TropFlux product until 3-4 months behind realtime, which should be available in 2012. 
    1111 
    12 TropFlux is largely derived from a combination of ERA-I re-analysis data for turbulent and longwave fluxes, and ISCCP surface radiation data for shortwave flux. All input products are bias- and amplitude-corrected on the basis of Global Tropical Moored Buoy Array data, before surface net heat flux and wind stresses are computed using the COARE v3 bulk algorithm. A precise description of the flux computation procedure, as well as a detailed evaluation against other timely, daily air-sea heat flux alternatives (OAFLUX, NCEP, NCEP2, ERA-I) is provided in Praveen Kumar et al. 2011. The wind stress product is described, evaluated and compared against other widely used products (QuikSCAT, NCEP, NCEP2, ERA-I) in Praveen Kumar et al. submitted 
     12TropFlux is largely derived from a combination of ERA-I re-analysis data for turbulent and longwave fluxes, and ISCCP surface radiation data for shortwave flux. All input products are bias- and amplitude-corrected on the basis of Global Tropical Moored Buoy Array data, before surface net heat flux and wind stresses are computed using the COARE v3 bulk algorithm. A precise description of the flux computation procedure, as well as a detailed evaluation against other timely, daily air-sea heat flux alternatives (OAFLUX, NCEP, NCEP2, ERA-I) is provided in Praveen Kumar et al. 2012. The wind stress product is described, evaluated and compared against other widely used products (QuikSCAT, NCEP, NCEP2, ERA-I) in Praveen Kumar et al. submitted 
    1313 
    1414We believe that this product offers the following advantages: 
     
    4848---------- 
    4949 
    50 Praveen Kumar, B., J. Vialard, M. Lengaigne, V. S. N. Murty, M. J. McPhaden, 2011: TropFlux: Air-Sea Fluxes for the Global Tropical Oceans - Description and evaluation, Climate Dynamics, 38, 1521-1543, doi:10.1007/s00382-011-1115-0 
     50Praveen Kumar, B., J. Vialard, M. Lengaigne, V. S. N. Murty, M. J. McPhaden, 2012: TropFlux: Air-Sea Fluxes for the Global Tropical Oceans - Description and evaluation, Climate Dynamics, 38, 1521-1543, doi:10.1007/s00382-011-1115-0 
    5151 
    52 Praveen Kumar, B., J. Vialard, M. Lengaigne, V.S.N. Murty, M. J. McPhaden, M.F. Cronin and F. Pinsard and K. Gopala Reddy, 2012: TropFlux wind stresses over the tropical oceans: evaluation and comparison with other products, submitted to Climate Dynamics  
     52Praveen Kumar, B., J. Vialard, M. Lengaigne, V. S. N. Murty, M. J. McPhaden, M.F. Cronin and F. Pinsard and K. Gopala Reddy, 2012: TropFlux wind stresses over the tropical oceans: evaluation and comparison with other products, submitted to Climate Dynamics  
  • trunk/adm/website/data_access.rst

    r147 r186  
    9292contact e-mail and a short sentence on how you plan to use the data. 
    9393 
    94 Please cite |pkbetal2011|_ in any publication using the heat flux data and  
    95 |pkbetal2012|_ in any paper using the wind stress data.  
     94Please cite |pkbetal2012|_ in any publication using the heat flux data and  
     95|pkbetal2012b|_ in any paper using the wind stress data.  
    9696Please acknowledge us by using the following sentence:  
    9797**The TropFlux data is produced under a collaboration between  
  • trunk/adm/website/description.rst

    r146 r186  
    6666    |gtma|_ 
    6767    data, despite systematic biases and underestimated variability 
    68     |pkbetal2011|_. 
     68    |pkbetal2012|_. 
    6969    The |isccpbrowse|_ provides the best shortwave data. 
    7070    **TropFlux hence uses bias and amplitude corrected ERA-I (10m-winds, 2m-air 
     
    7575    |gtma|_ 
    7676    data, and are described in detail in 
    77     |pkbetal2011|_. 
     77    |pkbetal2012|_. 
    7878 
    7979  * **An additional climatological surface temperature-dependent gustiness 
     
    9090    eastern equatorial Pacific and Atlantic oceans, but is in any case better 
    9191    than most available re-analyses in those regions  
    92     (|pkbetal2011|_). 
     92    (|pkbetal2012|_). 
    9393    The net surface shortwave that is provided in TropFlux data files is based 
    9494    on ISCCP data over the entire period for which it is available (July 1983 
  • trunk/adm/website/motivation.rst

    r146 r186  
    9696  * Air-sea fluxes obtained from re-analyses generally suffer from systematic 
    9797    biases, and do not perform extremely well for surface shortwave 
    98     fluxes (|pkbetal2011|_) 
     98    fluxes (|pkbetal2012|_) 
    9999 
    100100  * The |oaflux|_ project is a very useful initiative that delivers high-quality surface heat 
  • trunk/adm/website/overview.rst

    r147 r186  
    8585detailed evaluation against other timely, daily air-sea heat flux 
    8686alternatives (OAFLUX, NCEP, NCEP2, ERA-I) is provided in 
    87 |pkbetal2011|_. 
     87|pkbetal2012|_. 
    8888The wind stress product is described, evaluated and compared against other 
    8989widely used products (QuikSCAT, NCEP, NCEP2, ERA-I) in 
    90 |pkbetal2012|_ 
     90|pkbetal2012b|_ 
    9191 
    9292We believe that this product offers the following advantages: 
  • trunk/adm/website/prolog.rst

    r139 r186  
    2121.. $URL$ 
    2222.. 
     23.. - fplod 20120412 
     24.. 
     25..   * published paper new year 
     26.. 
    2327.. - fplod 20120222 
    2428.. 
     
    2731.. - 
    2832 
    29 .. |pkbetal2011| replace:: Praveen Kumar et al. 2011 
    30 .. _pkbetal2011: http://www.locean-ipsl.upmc.fr/~tropflux/papers/TropFlux_paper_accepted_r.pdf 
    31 .. |pkbetal2012| replace:: Praveen Kumar et al. submitted 
    32 .. _pkbetal2012: http://www.locean-ipsl.upmc.fr/~tropflux/papers/tropflux_stress_submitted_r.pdf 
     33.. |pkbetal2012| replace:: Praveen Kumar et al. 2012 
     34.. _pkbetal2012: http://www.locean-ipsl.upmc.fr/~tropflux/papers/TropFlux_paper_accepted_r.pdf 
     35.. |pkbetal2012b| replace:: Praveen Kumar et al. submitted 
     36.. _pkbetal2012b: http://www.locean-ipsl.upmc.fr/~tropflux/papers/tropflux_stress_submitted_r.pdf 
    3337.. |gtma| replace:: Global Tropical Moored Buoy Array 
    3438.. _gtma: http://www.pmel.noaa.gov/tao/global/global.html 
  • trunk/adm/website/selected_results.rst

    r161 r186  
    7676++++++++++++++++++++++++++++++++++ 
    7777 
    78 In |pkbetal2011|_ and |pkbetal2012|_, we have evaluated various widely 
     78In |pkbetal2012|_ and |pkbetal2012b|_, we have evaluated various widely 
    7979used surface heat flux / wind stress products (TropFlux, NCEP, NCEP2, 
    8080ERA-I and OAFLUX / QuikSCAT) against surface fluxes derived from 
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