@Article{BaņosMaGeSaCaNa:2022: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 a
convective storm case study",
journal = "Geoscientific Model Development",
year = "2022",
volume = "15",
number = "17",
pages = "6891--6917",
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 hybrid three-dimensional ensemble-variational
data assimilation (3DEnVar) algorithm in 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. A domain of 3 km horizontal grid spacing
is configured, and hourly update cycles are performed using
initial and lateral boundary conditions from the 3 km grid
High-Resolution Rapid Refresh (HRRR). Results show that a baseline
RRFS run is able to represent the observed convection, although
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 25 % of the static BEC with the supersaturation removal
function activated in GSI. Decreasing the vertical ensemble
localization radius from 3 layers to 1 layer in the first 10
layers of the hybrid analysis results in overall less skillful
forecasts. Convection is greatly improved when using planetary
boundary layer pseudo-observations, especially at 4h forecast, and
the bias of the 2 h forecast of temperature is reduced below 800
hPa. 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 the current
capabilities of the RRFS data assimilation system and identify
configurations that should be considered as candidates for the
first version of RRFS.",
doi = "10.5194/gmd-15-6891-2022",
url = "http://dx.doi.org/10.5194/gmd-15-6891-2022",
issn = "1991-959X",
label = "lattes: 8285827971934692 4 BaņosMaGeSaCaNa:2021:AsDaAs",
language = "en",
targetfile = "gmd-15-6891-2022.pdf",
urlaccessdate = "19 maio 2024"
}