@Article{NobreVendBast:2021:ImEnDa,
author = "Nobre, Jo{\~a}o Pedro Gon{\c{c}}alves and Vendrasco, {\'E}der
Paulo and Bastarz, Carlos Frederico",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)}",
title = "Impact of ensemble-variational data assimilation in heavy rain
forecast over brazilian northeast",
journal = "Atmosphere",
year = "2021",
volume = "12",
number = "9",
pages = "e1201",
month = "Sept.",
keywords = "3DEnVar, GSI, Mesoscale convective systems, WRF.",
abstract = "The Brazilian Northeast (BNE) is located in the tropical region of
Brazil. It is bounded by the Atlantic Ocean, and its climate and
vegetation are strongly affected by continental plateaus. The
plateaus keep the humid air masses to the east and are responsible
for the rain episodes, and at the west side the northeastern
hinterland and dry air masses are observed. This work is a case
study that aims to evaluate the impact of updating the model
initial condition using the 3DEnVar (Three-Dimensional Ensemble
Variational) system in heavy rain episodes associated with
Mesoscale Convective Systems (MCS). The results were compared to
3DVar (Three-Dimensional Variational) and EnSRF (Ensemble Square
Root Filter) systems and with no data assimilation. The study
enclosed two MCS cases occurring on 14 and 24 January 2017. For
that purpose, the RMS (Regional Modeling System) version 3.0.0,
maintained by the Center for Weather Forecasting and Climate
Studies (CPTEC), used two components: the Weather Research and
Forecasting (WRF) mesoscale model and the GSI (Gridpoint
Statistical Interpolation) data assimilation system. Currently,
the RMS provides the WRF initial conditions by using 3DVar data
assimilation methodology. The 3DVar uses a climatological
covariance matrix to minimize model errors. In this work, the
3DEnVar updates the RMS climatological covariance matrix through
the forecast members based on the errors of the day. This work
evaluated the improvements in the detection and estimation of 24 h
accumulated precipitation in MCS events. The statistic index RMSE
(Root Mean Square Error) showed that the hybrid data assimilation
system (3DEnVar) performed better in reproducing the precipitation
in the MCS occurred on 14 January 2017. On 24 January 2017, the
EnSRF was the best system for improving the WRF forecast. In
general, the BIAS showed that the WRF initialized with different
initial conditions overestimated the 24 h accumulated
precipitation. Therefore, the viability of using a hybrid system
may depend on the hybrid algorithm that can modify the weights
attributed to the EnSRF and 3DVar matrix in the GSI over the
assimilation cycles.",
doi = "10.3390/atmos12091201",
url = "http://dx.doi.org/10.3390/atmos12091201",
issn = "2073-4433",
language = "en",
targetfile = "nobre_impact.pdf",
urlaccessdate = "19 maio 2024"
}