The Potential Role of the GPM in Activities at the Naval Research Laboratory Joe Turk and Jeff Hawkins Naval Research Laboratory Marine Meteorology Division.

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The Potential Role of the GPM in Activities at the Naval Research Laboratory Joe Turk and Jeff Hawkins Naval Research Laboratory Marine Meteorology Division Monterey, CA USA GPM Planning Workshop UMUC Conference Center May 16-18, 2001

Research Activities at the Marine Meteorology Division (MMD) Numerical Weather Prediction  Global spectral model - NOGAPS  Regional, relocatable coupled ocean-atmosphere models  Advanced data assimilation strategies Meteorological Satellite Data Applications  Near real-time, global environment for “on-scene” and nowcasting systems  NRL is a “development ground” for eventual transitions of applications to an operational status

Looking at the GPM from the NRL Perspective  Environmental Data Records (EDR) from the Special Sensor Microwave Imager (SSM/I) program since 1987 (SSMI/S and WindSat are the upcoming follow-on missions)  Requirements have shifted to a more regional scale anywhere on the globe (geostationary perspective)  NRL has focused on complementary geostationary and microwave-based applications (increasingly, NWP model data)  More frequent updates of microwave-based data would find use in nowcasting applications and model assimilation techniques

Use of TRMM Near Real-Time Data  NRL-developed Automated Tropical Cyclone Forecasting (ATCF) system used to drive an automated WWW dissemination of all new and active tropical storms (archive since 1998)  TRMM near-real time data is in routine usage at the Joint Typhoon Warning Center (JTWC) since early 1999  TMI enhances existing geostationary VIS/IR, SSM/I and scatterometer observations and has significantly improved the estimation and tracking of tropical cyclone intensity  Higher-resolution imagery, rain and wind speed are important  Blending geostationary and low-Earth orbiting microwave data

Tropical Cyclone Web Page

2nd Eyewall forming Concentric Eyewalls

2nd Eyewall forming

Capturing Rapidly-Evolving Rain Events Basic Principle and Methodology  GEO: rapid-update, fine-scale, IR-based  LEO: infrequent time-update, coarse scale, microwave-based  Accumulate regional probability-matched histograms of time/space-coincident IR and rain measurements, dynamically Limitations  The limited number of MW-based satellite sensors  At shorter time scales, the temporal information is nearly all from the IR  Time gaps between successive microwave overpasses relative to the time scale of the storm evolution  Orographically-based events  Artifacts in the microwave data (snow, poor geolocation, etc.)

How many hours ago did the last microwave-based update occur? (F-13/14/15, TMI) Global geostationary IR composite at 2001/05/ UTC

12-hour accumulations at 2001/05/ UTC – blended technique 12-hour accumulations at 2001/05/ UTC – microwave only (F-13/14/15, TMI)

Research Activities and Plans Precipitation Validation  Korean Peninsula (1-minute reporting gauge dataset)  Australian national network (daily totals)  Comparisons with other geostationary-based techniques New Data Sources  Currently investigating the addition of AMSU data to increase the frequency of microwave-based overpasses  Additional use of NWP model data to “smarten” the blended satellite rain technique NWP Applications Cloud LWC data assimilation ( time frame)