Recent Changes

Tuesday, October 17

  1. file porva2.html uploaded
    5:51 pm
  2. page CMORPH edited work in progress! Accordion Section 1 Lorem ipsum dolor sit amet, consectetur adipisicing elit,…
    work in progress!
    Accordion
    Section 1
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    Section 2
    Lorem ipsum dolor sit amet, consectetur adipisicing elit, sed do eiusmod tempor incididunt ut labore et dolore magna aliqua. Ut enim ad minim veniam, quis nostrud exercitation ullamco laboris nisi ut aliquip ex ea commodo consequat.
    Section 3
    Lorem ipsum dolor sit amet, consectetur adipisicing elit, sed do eiusmod tempor incididunt ut labore et dolore magna aliqua. Ut enim ad minim veniam, quis nostrud exercitation ullamco laboris nisi ut aliquip ex ea commodo consequat.
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    NOAA CPC MORPHing technique: high resolution precipitation (60S-60N) v1.0
    CMORPH produces global precipitation analyses at very high spatial and temporal resolution. This technique uses precipitation estimates that have been derived from low orbiter satellite microwave observations exclusively, and whose features are transported via spatial propagation information that is obtained entirely from geostationary satellite IR data.
    (view changes)
    5:27 pm
  3. page CMORPH edited work in progress! Accordion Section 1 Lorem ipsum dolor sit amet, consectetur adipisicing elit,…
    work in progress!
    Accordion
    Section 1
    Lorem ipsum dolor sit amet, consectetur adipisicing elit, sed do eiusmod tempor incididunt ut labore et dolore magna aliqua. Ut enim ad minim veniam, quis nostrud exercitation ullamco laboris nisi ut aliquip ex ea commodo consequat.
    Section 2
    Lorem ipsum dolor sit amet, consectetur adipisicing elit, sed do eiusmod tempor incididunt ut labore et dolore magna aliqua. Ut enim ad minim veniam, quis nostrud exercitation ullamco laboris nisi ut aliquip ex ea commodo consequat.
    Section 3
    Lorem ipsum dolor sit amet, consectetur adipisicing elit, sed do eiusmod tempor incididunt ut labore et dolore magna aliqua. Ut enim ad minim veniam, quis nostrud exercitation ullamco laboris nisi ut aliquip ex ea commodo consequat.
    Lorem ipsum...
    Section 2
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    Section 3
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    NOAA CPC MORPHing technique: high resolution precipitation (60S-60N) v1.0
    CMORPH produces global precipitation analyses at very high spatial and temporal resolution. This technique uses precipitation estimates that have been derived from low orbiter satellite microwave observations exclusively, and whose features are transported via spatial propagation information that is obtained entirely from geostationary satellite IR data.
    (view changes)
    5:27 pm
  4. 5:23 pm
  5. page CMORPH edited work in progress! NOAA CPC MORPHing technique: high resolution precipitation (60S-60N) v1.0

    work in progress!
    NOAA CPC MORPHing technique: high resolution precipitation (60S-60N) v1.0
    (view changes)
    4:26 pm
  6. page CMORPH edited work in progress! NOAA CPC MORPHing technique: high resolution precipitation (60S-60N) v1.0 C…

    work in progress!
    NOAA CPC MORPHing technique: high resolution precipitation (60S-60N) v1.0
    CMORPH produces global precipitation analyses at very high spatial and temporal resolution. This technique uses precipitation estimates that have been derived from low orbiter satellite microwave observations exclusively, and whose features are transported via spatial propagation information that is obtained entirely from geostationary satellite IR data.
    The grid resolution is 0.07277 degrees lat/lon (8 km at the equator) and temporal resolution is 30 minutes. With regard to spatial resolution, although the precipitation estimates are available on a grid with a spacing of 8 km (at the equator), the resolution of the individual satellite-derived estimates is coarser than that - more on the order of 12 x 15 km or so. The finer "resolution" is obtained via interpolation. (source CPC website )
    ...
    ftp server.
    More information is available on the CPC website and the data climate guide website .
    Terms of use
    (view changes)
    4:25 pm

Monday, October 2

  1. page Unified Model edited ... If a run fails, search for 'UM ERROR' in the .leave file to see what went wrong. Common issues…
    ...
    If a run fails, search for 'UM ERROR' in the .leave file to see what went wrong. Common issues are listed here
    REPLANCA: PP HEADERS ON ANCILLARY FILE DO NOT MATCH
    Known UM failures at UKMO
    Job Input
    UM Ancillary files
    (view changes)
    5:51 pm
  2. page Unified Model edited ... ARCCSS researchers need to email climate_help@nci.org.au to request an account on the Met Offi…
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    ARCCSS researchers need to email climate_help@nci.org.au to request an account on the Met Office server.
    Supported Experiments
    ...
    Atmosphere' (GA) NCI configurations at NCI
    Nesting Suite
    Experiments in Preparation
    (view changes)
    5:44 pm
  3. page Unified Model edited The Unified Model is the atmospheric component of ACCESS, developed by the UK's Met Office. The Cen…
    The Unified Model is the atmospheric component of ACCESS, developed by the UK's Met Office. The Centre of Excellence sublicences the UM from CAWCR, our licence allows us to run the UM at NCI only. To run the UM you will first need an NCI account, then ask for connection to the ACCESS group through NCI's account website.
    The ACCESS climate models are based on version 7.3 of the UM, most Australian university research uses this version. The Bureau makes use of the more recent version 7.8 for forecasting, and is evaluating moving to version 8.2. These are the primary versions supported at NCI, other versions are available but may not be quite as well tested. Different versions include changed science configurations, for details see the changelog.
    = GettingGetting Started
    The UM is configured through a graphical interface, which is run from the server accessdev.nci.org.au. See Setting up the environment for how to connect.
    Unified Model User's Guide
    (view changes)
    5:44 pm

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