Global Ozone and Surface UV Climatology Data Products for NASA Earth Observations (NEO) and Science on the Sphere (SOS) 1) Tropospheric Column Ozone in.

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Presentation transcript:

Global Ozone and Surface UV Climatology Data Products for NASA Earth Observations (NEO) and Science on the Sphere (SOS) 1) Tropospheric Column Ozone in Dobson Units 2) Stratospheric Column Ozone in Dobson Units 3) Total Column Ozone in Dobson Units 4) Surface UV-Index (These four data products represent 12-month climatologies with horizontal resolution of 1 o latitude by 1.25 o longitude) Contact person: Dr. Jerry Ziemke, Code 614 Ph:

The Data Arrays Given as a small IDL save file (slightly under 10 Mbytes) – in IDL type restore, ’global_ozone_uv_climatology_data_arrays.sav’ The IDL save file can be obtained from the following: > ftp jwocky.gsfc.nasa.gov > Name: anonymous > Password: > cd pub/ccd > get global_ozone_uv_climatology_data_arrays.sav

Global Tropospheric Column Ozone Climatology in Dobson Units Derived from Aura OMI v8.5 Total Column Ozone Minus Aura MLS v3.3 Stratospheric Column Ozone for Oct2004 through Jan2011 Uses WMO/NCEP 2K/km lapse rate tropopause pressure to separate tropospheric from stratospheric column ozone There is missing data in polar night latitudes including additional measurements at high latitudes/high solar zenith angles flagged as missing because of questionable data quality

Global Stratospheric Column Ozone Climatology in Dobson Units Derived from Aura MLS v3.3 ozone profile measurements from October 2004 through January 2011 Uses WMO/NCEP 2K per km lapse rate tropopause pressure definition to derive stratospheric column ozone Missing MLS data within a few degrees of latitude from the poles are filled in using extrapolated MLS measurements from nearby lower latitudes

Global Total Column Ozone Climatology in Dobson Units Derived from Aura OMI v8.5 measurements everywhere except in polar night latitudes For polar night latitudes, MLS v3.3 stratospheric column ozone is about 90-95% of total column ozone – the tropospheric column ozone product is extrapolated from lower latitudes and then added to MLS stratospheric column ozone to give a close estimate of total column ozone in polar night latitudes (result: total column ozone is an entire global map for each month, just like MLS stratospheric column ozone)

Global UV Index Climatology Derived directly from the total column ozone climatology product Derived using a UV-Index source code from P. Newman [e.g., Newman and McKenzie, 2011, Photochem. Photobiol. Sci.] which converts total column ozone and solar zenith angle at a fixed grid point to a single UV Index number The UV-Index maps include adjustments for both local terrain altitude and also the time-averaged Earth-Sun distance for each of the months of the climatology

Extra Slides

Adjustment of Surface UV for Earth-Sun Distance Exact Analytical Solution To General Two-body Gravitational Problem Distance of Earth from Sun as Function of Time of Year Time averaged Earth-Sun Month distance (A.U.) January February March April May June July August September October November December