GSI |
GFS-GSM |
CFS |
HWRF |
DOCUMENTATION | NCEP/DTC | MoES |
GSI | GSI Documents and Publications (DTC) | |
GFS-GSM | Documentation (NCEP/EMC) References |
Performance of T254L64, T382L64 and GEFS Global Assimilation Forecast System (NCMRWF) - Monsoon-2008 (pdf), Monsoon-2009 (pdf),Monsoon-2010 (pdf),Monsoon-2012 (pdf) Experimental real-time multi-model ensemble (MME) prediction of rainfall during monsoon 2008: Large-scale medium-range aspects (pdf) (NCMRWF) |
CFS | Documentation (NCEP/EMC) | Development of Extended range prediction system using CFSv2 and its verification - Report(pdf) |
Parallel Convention | <-- | Operational Convention | ||
biascr.CDUMP.CDATE | <-- | CDUMP.tCCz.abias | A, N | CDATE = YYYYMMDDCC (year, month, day, cycle), CC = cycle CDUMP = dump (gdas1 or gfs) A - required if cycling with analysis F - required if running forecast N - not available for gfs dump |
satang.CDUMP.CDATE | <-- | CDUMP.tCCz.satang | A, N | |
sfcanl.CDUMP.CDATE | <-- | CDUMP.tCCz.sfcanl | A, F | |
siganl.CDUMP.CDATE | <-- | CDUMP.tCCz.sanl | A, F |
Parallel Convention | <-- | Operational Convention | CDATE = YYYYMMDDCC (year, month, day, cycle), CC = cycle A - required if cycling with analysis F - required if running forecast | |
biascr.gdas.CDATE | <-- | cdas1.tCCz.abias | A | |
satang.gdas.CDATE | <-- | cdas1.tCCz.satang | A | |
sfcanl.gdas.CDATE | <-- | cdas1.tCCz.sfcanl | A, F | |
siganl.gdas.CDATE | <-- | cdas1.tCCz.sanl | A, F | |
ocnanl.gdas.CDATE.tar | <-- | cdas1.tCCz.ocnanl.tar | A, F |
3D/4D-Var | Three/Four Dimensional Varioational Method (for data asssimilation) |
4DDA | Four Dimensional Data Assimilation (for data asssimilation) |
AC | Anomaly Correlation |
CFS | Climate Forecast System |
CFSv2 | Climate Forecast System version 2.0.0 |
CPC | Climate Prediction Center (NCEP) - visit website |
DTC | Developmental Testbed Center (Boulder, CO) - visit website |
ECMWF | European Centre for Medium-Range Weather Forecasts, Europe - visit website |
EMC | Environmental Modeling Center (NCEP) - visit website |
EnKF | Ensemble Kalman Filter (data asssimilation method) |
ESSO | Earth System Sciences Organisation, India |
GDAS | Global Data Assimilation System, the late run of the GFS, a short 9-hr forecast utilizing late arriving data, provides guess fields / initial conditions for next GFS cycle. Example: 18z GDAS provides initial conditions for 00z GFS |
GFS | Global Forecast System (entire suite of systems: GSI, GSM, CFS), commonly used to refer to forecast output from entire coupled system although forecast actually comes from the GSM |
GSI | Gridpoint Statistical Interpolation, GFS data assimilation system |
GSM | Global Spectral Model, forecast model in GFS |
HWRF | Hurricane Weather Research and Forecast System - visit website |
IC(s) | initial condition(s) for model |
IITM | Indian Institute of Tropical Meteorology - visit website |
IMD | India Meteorological Department - visit website |
INCOIS | Indian National Centre for Ocean Information Services - visit website |
MISO | monsoon intraseasonal oscillations - visit website |
MoES | Ministry of Earth Sciences, India - visit website |
MOK | Monsoon over Kerala, onset of Monsoon in India - visit website |
MOM4 | Modular Ocean Model is the Ocean Model in GFS, developed by GFDL - visit website |
NCEP | National Centres for Environmental Prediction, USA - visit website |
NCMRWF | National Centre for Medium Range Weather Forecasting (Noida, India) - visit website |
NOMADS | NOAA National Operational Model Archive and Distribution System (NOMADS) is a Web-services based project providing both real-time and retrospective format independent access to climate and weather model data |
T574 | Triangular Spectral truncation. Domain shape is in spectral space and traingular is isotropic on sphere. 574 is the maximum number of waves around a great circle in any direction ; so the shortest wavelength is 40,000/574 = 70 km. Eulerian Global Spectral Model (GSM) uses 3 gridpoints per wave, on tranform grid of "1760 X 880" reduced Gaussian grid. The horizontal resolution at T574 becomes ~ 23 km |
T382 | Spectral truncation equivalent to horizontal resolution ~37 km |
T254 | Spectral truncation equivalent to horizontal resolution ~50-55 km |
T190 | Spectral truncation equivalent to horizontal resolution ~70 km |
T126 | Spectral truncation equivalent to horizontal resolution ~100 km |
UM | Unified Model by British Met Office, UK - visit website |