@Article{BaņosMaGeSaCaNa:2021:AsDaAs,
author = "Baņos, Ivette Hernandes and Mayfield, Will D. and Ge, Guoqing and
Sapucci, Luiz Fernando and Carley, Jacob R. and Nance, Louisa",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {National
Center for Atmospheric Research} and {NOAA Global Systems
Laboratory} and {Instituto Nacional de Pesquisas Espaciais (INPE)}
and {NOAA/NCEP Environmental Modeling Center} and {National Center
for Atmospheric Research}",
title = "Assessment of the data assimilation framework for the Rapid
Refresh Forecast System v0.1 and impacts on forecasts of
convective storms",
journal = "Geoscientific Model Development Discussions",
year = "2021",
volume = "2021",
number = "36",
pages = "1",
keywords = "Data assimilation, Convective process, Rapid Refresh Forecast
System.",
abstract = ". The Rapid Refresh Forecast System (RRFS) is currently under
development and aims to replace the National Centers for
Environmental Prediction (NCEP) operational suite of regional and
convective scale modeling systems in the next upgrade. In order to
achieve skillful forecasts comparable to the current operational
suite, each component of the RRFS needs to be configured through
exhaustive testing and evaluation. The current data assimilation
component uses the Gridpoint Statistical Interpolation (GSI)
system. In this study, various data assimilation algorithms and
configurations in GSI are assessed for their impacts on RRFS
analyses and forecasts of a squall line over Oklahoma on 4 May
2020. Results show that a baseline RRFS run without data
assimilation is able to represent the observed convection, but
with stronger cells and large location errors. With data
assimilation, these errors are reduced, especially in the 4 and 6
h forecasts using 75 % of the ensemble background error covariance
(BEC) and with the supersaturation removal function activated in
GSI. Decreasing the vertical ensemble localization radius in the
first 10 layers of the hybrid analysis results in overall less
skillful forecasts. Convection and precipitation are overforecast
in most forecast hours when using planetary boundary layer
pseudo-observations, but the root mean square error and bias of
the 2 h forecast of 2 m dew point temperature are reduced by 1.6 K
during the afternoon hours. Lighter hourly accumulated
precipitation is predicted better when using 100 % ensemble BEC in
the first 4 h forecast, but heavier hourly accumulated
precipitation is better predicted with 75 % ensemble BEC. Our
results provide insight into current capabilities of the RRFS data
assimilation system and identify configurations that should be
considered as candidates for the first version of RRFS.",
issn = "1991-962X and 1991-9611",
label = "lattes: 8285827971934692 4 BaņosMaGeSaCaNa:2021:AsDaAs",
language = "en",
targetfile = "banos_assessment.pdf",
url = "https://gmd.copernicus.org/preprints/gmd-2021-289/",
urlaccessdate = "19 maio 2024"
}