J1.3 The Global Hydro-Intelligence Subseasonal-to-Seasonal (GHI-S2S) Forecast System

Monday, 29 January 2024: 9:00 AM
Holiday 6 (Hilton Baltimore Inner Harbor)
Kristi R. Arsenault, GSFC, Greenbelt, MD; SAIC, Reston, VA; and R. A. Zamora, S. Mahanama, J. W. Wegiel, S. V. Kumar, PhD, E. M. Kemp, A. Getirana, Y. Yoon, A. Hazra, M. Navari, D. M. Mocko, and R. A. Wade

Handout (7.6 MB)

Producing reliable and timely global hydrometeorological forecasts on subseasonal-to-seasonal timescales is a significant need of many government agencies, companies and operating centers, especially in relation to disseminating near real-time drought and flood potential information and making life-saving decisions. To help meet this need, the Global Hydro-Intelligence Subseasonal-to-Seasonal (GHI-S2S) system has been developed at NASA, which derives its skill from: (i) accurate initial conditions produced by an offline land modeling system through the assimilation of various satellite data; and (ii) an ensemble of meteorological forecast data produced by state-of-the-art ocean-land-atmosphere forecast systems. GHI-S2S uses NASA’s Land Information System (LIS) land modeling and hydrological framework, which employs a variety of ensemble and forecast capabilities along with improved initial land surface or hydrologic conditions for the forecasts, including assimilation of remotely sensed soil moisture data. GHI-S2S also utilizes precipitation hindcasts and forecasts from the North American Multi-Model Ensemble (NMME), and non-precipitation data (e.g., near-surface temperatures and winds) from NOAA’s Climate Forecast System, version 2 (CFSv2). GHI-S2S is configured for the full global domain (including Antarctica), producing daily and monthly hydrometeorological forecast fields out to nine lead months. A suite of output metrics and products for drought and flood potential prediction are generated both for hindcasts and routine forecast runs. We present real-world examples and verification of the system for different domains and hydrometeorological variables (e.g., soil moisture, terrestrial water storage and streamflow).
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