Handout (3.7 MB)
Satellite soundings struggle in the lower tropospheric region due to the increased opacity of the atmosphere. This is particularly true over land areas where surface dis-homogeneities and uncertainties in the surface emissivity penalize the accuracy of the lower tropospheric temperature and dewpoint temperature retrieval even further. Both parameters are key inputs to the computation of CAPE.
In this study, an investigation of the use of combined surface station data and NUCAPS profile data is conducted to create an accurate near-real time estimate of surface-based CAPE (SBCAPE). Hourly surface observations are matched up in space and time with NUCAPS vertical profiles to create a combined CAPE calculation using the SHARPpy tool. An automated process is used to calculate the SBCAPE on a 0.7x0.7 degree grid for each overpass of the Suomi-NPP satellite using the UW-Madison SSEC Direct Broadcast antennae. This innovative data fusion product will be compared to the operational NUCAPS-derived SBCAPE for validation. This comparison will serve as a baseline to evaluate future improvements in the NUCAPS retrieval system to better serve real time users applications over the CONUS region. A possible developmental solution for NUCAPS is the inclusion of these surface station data to better constrain the first guess regression solution of skin temperature. Future development plans include the validation of an experimental NUCAPS product, the 2-meter height temperature retrieval, for the computation of the mixed-layer CAPE (MLCAPE). Preliminary validation results will be presented at the conference using visualization tool, SSEC RealEarthTM, in near-real time (https://realearth.ssec.wisc.edu/).
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