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- Timestamp:
- 02/23/12 09:57:10 (12 years ago)
- Location:
- trunk/adm/website
- Files:
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- 7 edited
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bibliography_web.rst (modified) (1 diff)
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conf.py (modified) (3 diffs)
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data/changes.rst (modified) (2 diffs)
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data_access.rst (modified) (3 diffs)
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documentation.rst (modified) (1 diff)
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overview.rst (modified) (2 diffs)
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selected_results.rst (modified) (8 diffs)
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trunk/adm/website/bibliography_web.rst
r127 r140 4 4 .. ==== 5 5 .. 6 .. connexion with superbib so will be replaced by file:`bibtropflux.xml` 6 .. connexion with superbib so will be replaced by file:`bibtropflux.xml` (action fp) 7 7 .. 8 8 .. EVOLUTIONS 9 9 .. ========== 10 10 .. 11 .. $Id$ 12 .. 11 13 .. $URL$ 12 ..13 .. $Id$14 14 .. 15 15 .. - fplod 20111107T090527Z aedon.locean-ipsl.upmc.fr (Darwin) -
trunk/adm/website/conf.py
r139 r140 24 24 # 25 25 # $URL$ 26 # 27 # - fplod 20120223 28 # 29 # * fix syntax error for exclude prolog.rst 26 30 # 27 31 # - fplod 20120222 … … 30 34 # * add rst_prolog 31 35 # thanks to https://github.com/leaflabs/leaflabs-docs/blob/master/source/conf.py 32 #33 36 # 34 37 # - fplod 20120221 … … 131 134 # List of patterns, relative to source directory, that match files and 132 135 # directories to ignore when looking for source files. 133 exclude_patterns = ['_build' 'prolog.rst']136 exclude_patterns = ['_build', 'prolog.rst'] 134 137 135 138 # Included at the beginning of every source file that is read. -
trunk/adm/website/data/changes.rst
r139 r140 22 22 .. 23 23 .. $URL$ 24 .. 25 .. - fplod 20120223 26 .. 27 .. * typo 24 28 .. 25 29 .. - fplod 20120222 … … 60 64 ======= 61 65 62 Following information are provided to emphas e modification that may66 Following information are provided to emphasise modification that may 63 67 may have impacts on tools using TropFlux products. 64 68 -
trunk/adm/website/data_access.rst
r139 r140 15 15 .. ==== 16 16 .. 17 .. 17 .. Comment fait-on les accents (I R Develop° (jv) 18 18 .. 19 19 .. EVOLUTIONS … … 23 23 .. 24 24 .. $URL$ 25 .. 26 .. - fplod 20120223 27 .. 28 .. * typo + split long lines 25 29 .. 26 30 .. - fplod 20120222 … … 79 83 contact e-mail and a short sentence on how you plan to use the data. 80 84 81 Please cite |pkbetal2011|_ in any publication using the heat flux data and |pkbetal2012|_ in any paper using the wind stress data. Please acknowledge us by using the following sentence: **The TropFlux data is produced under a collaboration between Institut Pierre Simon Laplace (IPSL, Paris, France) and National Institute of Oceanography/CSIR (NIO, Goa, India), and supported by Instititut de Recherche pour le Developpement (IRD, France). TropFlux relies on data provided by the ECMWF Re-Analysis interim (ERA-I) and ISCCP projects.** 85 Please cite |pkbetal2011|_ in any publication using the heat flux data and 86 |pkbetal2012|_ in any paper using the wind stress data. 87 Please acknowledge us by using the following sentence: 88 **The TropFlux data is produced under a collaboration between 89 Institut Pierre Simon Laplace (IPSL, Paris, France) and 90 National Institute of Oceanography/CSIR (NIO, Goa, India), and 91 supported by Institut de Recherche pour le Developpement (IRD, France). 92 TropFlux relies on data provided by the ECMWF Re-Analysis interim (ERA-I) 93 and ISCCP projects.** 82 94 83 95 Please keep us informed of any published paper that makes use of this data. -
trunk/adm/website/documentation.rst
r139 r140 44 44 ============= 45 45 46 The following papers present the TropFlux data 46 The following papers present the TropFlux data : 47 47 48 48 - 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, on line, `doi:10.1007/s00382-011-1115-0 <http://dx.doi.org/10.1007/s00382-011-1115-0>`_, `TropFlux_paper_accepted_r.pdf <http://www.locean-ipsl.upmc.fr/~tropflux/papers/TropFlux_paper_accepted_r.pdf>`_ -
trunk/adm/website/overview.rst
r139 r140 17 17 .. 18 18 .. $URL$ 19 .. 20 .. - fplod 20120223 21 .. 22 .. * typo 19 23 .. 20 24 .. - fplod 20120222 … … 99 103 `National Institute of Oceanography/CSIR <http://www.nio.org/>`_, India. 100 104 Bilateral scientific visits to France and India have been supported by 101 `Institut de Recherche pour le D eveloppement <http://www.ird.fr/>`_, France.105 `Institut de Recherche pour le Développement <http://www.ird.fr/>`_, France. 102 106 -
trunk/adm/website/selected_results.rst
r139 r140 24 24 .. 25 25 .. $URL$ 26 .. 27 .. - fplod 20120223 28 .. 29 .. * split long lines + one type 26 30 .. 27 31 .. - fplod 20120222 … … 57 61 ++++++++++++++++++++++++++++++++++ 58 62 59 In |pkbetal2011|_ and |pkbetal2012|_, we have evaluated various widely used surface heat flux / wind stress products (TropFlux, NCEP, NCEP2, ERA-I and OAFLUX / QuikSCAT) against surface fluxes derived from |gtma|_ data. While this does not constitute an independent validation (most of these products use |gtma|_ data in their derivation), this is at least a test of the capacity of each product to fit the largest repository of air-sea flux data in the tropics. 63 In |pkbetal2011|_ and |pkbetal2012|_, we have evaluated various widely 64 used surface heat flux / wind stress products (TropFlux, NCEP, NCEP2, 65 ERA-I and OAFLUX / QuikSCAT) against surface fluxes derived from 66 |gtma|_ data. 67 While this does not constitute an independent validation (most of these 68 products use |gtma|_ data in their derivation), this is at least a test 69 of the capacity of each product to fit the largest repository of air-sea 70 flux data in the tropics. 60 71 61 72 .. figure:: correlation.png … … 65 76 Caption figure 1 : correlation and rms-difference of various daily net 66 77 heat flux / wind stress module products to 67 global tropical moored buoy array daily data (computed at each site and then averaged across the sites). 78 global tropical moored buoy array daily data (computed at each site 79 and then averaged across the sites). 68 80 69 Figure 1 shows that, for both wind stress and net heat fluxes, TropFlux is the product that 81 Figure 1 shows that, for both wind stress and net heat fluxes, TropFlux is 82 the product that 70 83 displays the highest correlation and lowest rms-difference to observations 71 84 (closely followed by OAFlux heat fluxes and ERA-I wind stresses). 72 This is an indication of the very high accuracy of the Trop flux product.85 This is an indication of the very high accuracy of the TropFlux product. 73 86 Additional validations to independent data in 74 87 |pkbetal2011|_ … … 76 89 |pkbetal2012|_ 77 90 also seem to suggest that TropFlux is amongst the most accurate tested products. 78 79 91 80 92 Tropical climate mean state and variability from TropFlux … … 112 124 :width: 80% 113 125 114 Caption figure 4 : Standard deviation of TropFlux net heat flux monthly anomalies115 with respect to the mean seasonal cycle (1989-2010).126 Caption figure 4 : Standard deviation of TropFlux net heat flux monthly 127 anomalies with respect to the mean seasonal cycle (1989-2010). 116 128 117 129 .. figure:: std_taux_ano_1989_2010_website.jpg … … 120 132 :width: 80% 121 133 122 Caption figure 5 : Standard deviation of TropFlux wind stress monthly anomalies123 with respect to the mean seasonal cycle (1989-2010).134 Caption figure 5 : Standard deviation of TropFlux wind stress monthly 135 anomalies with respect to the mean seasonal cycle (1989-2010). 124 136 125 Figures 4 and 5 show low frequency non-seasonal variability (i.e. interannual variability). 137 Figures 4 and 5 show low frequency non-seasonal variability (i.e. interannual 138 variability). 126 139 There is of course increased variance toward mid-latitudes due to the effect 127 of midlatitude stochastic forcing. But interannual wind stress and heat flux 140 of midlatitude stochastic forcing. 141 But interannual wind stress and heat flux 128 142 variations associated with the El Niño phenomenon are very clear close to 129 143 the equator and dateline. … … 133 147 134 148 Intraseasonal variability 135 +++++++++++++++++++++++++ ++++++++++++++++++++++++++++++++149 +++++++++++++++++++++++++ 136 150 137 151 .. figure:: interseasonal.png 138 :alt: Wind stress and net heat flux perturbations associated with monsoon active/break phases. 152 :alt: Wind stress and net heat flux perturbations associated with monsoon 153 active/break phases. 139 154 :align: center 140 155 141 Caption figure 6 : 7-day low-passed a) Outgoing longwave radiation (a proxy of deep 156 Caption figure 6 : 7-day low-passed a) Outgoing longwave radiation (a proxy 157 of deep 142 158 atmospheric convection), b) wind stress and c) net air-sea flux at 143 159 the 15°N, 90°E RAMA mooring during the 2009 monsoon. … … 149 165 fluxes estimates (thick, red curve) and estimates from the 150 166 other products in various colors. 151 The root-mean square difference of each product with TPR is indicated on panel152 b (in :math:`N.m^-2`) and c (in :math:`W.m^-2`).167 The root-mean square difference of each product with TPR is indicated on 168 panel b (in :math:`N.m^-2`) and c (in :math:`W.m^-2`). 153 169 154 170 Finally, figure 6 is an illustration of intraseasonal surface
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