---TITLE: ISCCP Cloud and Radiative Flux in 50km ARCMIP-EASE Grid 199709-199809 ---AUTHORS: Prof. Judith Curry School of Earth and Atmospheric Sciences Georgia Institute of Technology Atlanta, GA 30332-0340 Phone: (404) 894-3955 Fax: (404) 894-5638 Email: curryja@eas.gatech.edu Yuanchong Zhang Goddard Institute for Space Studies 2880 Broadway, RM 320-B New York, NY 10025 Phone: (212) 678-5514 Fax: (212) 678-5552 Email: clyxz@giss.nasa.gov Contact for data questions : Mathew V. Rothstein Program in Atmospheric and Oceanic Sciences University of Colorado Boulder, CO 80309 Phone: (303) 492-4035 Email: Mathew.Rothstein@colorado.edu Randolph A. Reeder Aerospace Engineering Dept. University of Colorado Boulder, CO 80309 Phone: (303) 492-4266 Email: rreeder@cloud.colorado.edu ---DATA SET OVERVIEW: The ISCCP Cloud and Radiative Flux data set is a subset of ISCCP's FDX-P2 Sheba Flux Data set regridded into a 50km EASE-Grid. It contains surface and top-of-atmosphere radiative fluxes and the important physical quantities used to calculate them. The data set covers the time period of September, 1997 through September, 1998, which is roughly coincident with that of the SHEBA project. Spatial coverage includes the polar region of 55N to the North Pole. Temporal resolution is every 3hrs. There are two satellites available for the period: The NOA-14 afternoon (NOA) and NOA-12 morning (NOM) polar orbiters. For more information on ISCCP and their products visit: http://isccp.giss.nasa.gov/ For information on EASE-Grid visit: http://www-nsidc.colorado.edu/data/ease/ ---INSTRUMENT DESCRIPTION: The following is an excerpt from the ISCCP FDX-P2 readme file: Shortwave and Longwave Radiative Flux are calculated using the following datasets to specify the properties of Earth's Atmosphere and Surface: ISCCP-DX cloud dataset, TOVS operational sounder products, TOMS ozone products, a climatology of near-surface air temperature diurnal cycle constructed from the WWW Surface Weather reports and the first NCEP reanalysis, a climatology of cloud particle sizes from Han et al, a climatology of stratospheric and upper tropospheric water vapor from SAGE-II, a climatology of tropospheric and stratospheric aerosols used in the GISS climate model, and land surface albedo spectral dependence and spectral emissivities from the GISS climate model. ---DATA FORMAT: The data are stored by two different methods for easy access. The first set of files contain all cloud and radiative flux variables by 3hr window. These files are named: cloud_yymmddhh.sat.nc and rflux_yymmddhh.sat.nc where yymmddhh is the timestamp, sat is the satellite of origin (NOA or NOM), and nc indicates these are self-documented NetCDF files. These files are tarred together by month and gzipped into files named: isccp_yymm.sat.tar.gz The second set of files store the data by variable and contain the entire period of record. These files are named: isccp_var.sat.nc.gz where var is a two to four letter abbreviation of the variables described below. As mentioned, all data are stored in NetCDF files, which contain additional detailed information as metadata. The basic storage format is a 161x161 grid corresponding to the inner-most square of the 50km ARCMIP-EASE projection of the northern hemisphere. Converting between this grid and the full 361x361 hemispheric grid is simply a matter of adding/ subtracting 100 to the column and row. A list of variables is provided here: radiative flux variables: swds SW downwelling at surface (W/m^2) swus SW upwelling at surface (W/m^2) lwds LW downwelling at surface (W/m^2) lwus LW upwelling at surface (W/m^2) swdt SW downwelling at TOA (W/m^2) swut SW upwelling at TOA (W/m^2) lwut LW upwelling at TOA (W/m^2) skin surface skin temperature (K) alb surface visible albedo (0-1) cloud variables: o3 column O3 (Dobson unit) pwc column PW actually used (cm) ctpr highest cloud layer top pressure (mb) actually used cbpr lowest cloud layer base pressure (mb) actually used tau total column Tau actually used ---DATA REMARKS: 1) Missing data are represented by -9999. 2) There was no data for the NOA satellite during Nov, 1997. 3) An error was detected in the Shortwave flux calculation over land. Therefore, all Shortwave values in land grid cells are treated as missing (-9999). 4) In the process of regridding, extreme outliers were omitted and linear averages used to determine a grid cell's value.