Workshop do DIMNT/CGCT/INPE, 6-7 de outubro de 2022
Assimilação de dados nas componentes do sistema Terrestre:
status e perspectivas futuras no contexto do MONAN
Assimilação de Dados Oceanográficos
com o Sistema HYCOM+RODAS: Status e Perspectivas
Clemente A. S. Tanajura (UFBA)
Filipe Bitencourt Costa (CHM e UFBA)
Geoff Souza Dorfschäfer (UFBA)
Leonardo Brito Pires (UFBA)
Janini Pereira (UFBA)
Vitor Fernando da Silva Vidal
Davi Mignac Carneiro (UK MetOffice)
Rafael Santana (University of Auckland))
Alex Novaes de Santana (SOCIB)
Leonardo Lima (CMCC)
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Content
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REMO is a research group
Research and technological development in operational oceanography and physical oceanography with focus on the South Atlantic and regions along the Brazilian coast using assimilative models and observational data. It was formed in 2007.
Products:
www.rederemo.org
Ensemble Optimal Interpolation (EnOI)
EnOI: B is estimated with model states from a free run
The REMO Ocean Data Assimilation System (RODAS) was constructed based on EnOI; M Ensemble members are not static (Xie and Zhu 2010, Tanajura et al 2014, Mignac et al 2015; Costa e Tanajura 2015; Carvalho et al. 2019; Tanajura et al. 2020, Santana et a;, 2020; Dorfschäfer et al. 2020; Costa e Tanajura 2022)
11 members
11 members
M = 132
Operational Ocean Forecast in REMO-CHM
HYCOM 1/4o 1/12o 1/24o with tides L21
Large-scale circulation in the Atlantic and downscaling to METAREA V and region along the Brazilian S-SE coast in the Brazilian Navy CHM operational system.
Brazilian Navy Hydrography Center (CHM) Operational System
Operational Ocean Forecast in REMO-CHM
Large-scale 1/12o domain increased, Metarea V domain now with 1/24o resolution L32 with tides.
HYCOM 1/12o 1/24o with tides L32
Mean SSH
This and the other nested system are running operationally today in CHM
HYCOM+RODAS 11-yr Reanalysis
UK MetOffice SST analysis (1/20º resolution)
SSH from CMEMS (gridded with 1/4º resolution)
T/S profiles from 13,988 XBTs, 1,718 CTDs, 8 PIRATA buoys and 45,325 Argo profilers.
Strategy to use synthetic S to pair single T XBT and PIRATA profiles
Dorfschäfer et al. JGR (2020)
HYCOM+RODAS 11-yr reanalysis
Locations of the in situ data assimilated in the reanalysis from January 1, 2008 to December 31, 2018. On the left, 13,988 XBTs are in red, 1,718 CTDs in green and 8 PIRATA buoys in blue. On the right, 45,325 Argo T/S profiles are in blue. (Tanajura et al. 2022, under preparation)
HYCOM+RODAS 11-yr reanalysis
SST RMSD (oC) with respect to OSTIA for the Control free run, reanalysis B_H_MV.2 and the COAPS/FSU HYCOM+NCODA system.
SST RMSD (oC)
HYCOM+RODAS 11-yr reanalysis
SST RMSD (oC)
SSH Correlation with respect to AVISO for the Control free run, reanalysis (B_H_MV.2) and the COAPS/FSU HYCOM+NCODA system.
HYCOM+RODAS 11-yr reanalysis
Control
Reanalysis
Control
Reanalysis
GLORYS
GLORYS
NCODA
NCODA
T RMSD (oC)
S RMSD
30 d Predictability Assessment
SST RMSD
SLA RMSD
SST Corr
SLA Corr
Free
Persistence
Hindcast
Carvalho J, Costa, FB, Mignac D, Tanajura CAS, JOO, 2019
48 30-d hindcasts were performed and compared with HYCOM+RODAS analyses
Persistence
Persistence
Persistence
Hindcast
Hindcast
Hindcast
Free
Free
Free
OSE with HYCOM+RODAS
Tanajura et al.,Ocean Dyn, 2020
Assess the relative importance of
OSTIA SST
AVISO SLA
Argo T/S
Meridional current on Feb 27, 2012, along the NOAA XBT line AX97
OSE with XBTs and Synthetic Salinity
Dorfshäfer et al., JGR, 2020
OSSE: Assimilation of SWOT SSH
SLA SWOT data: along-track on 2 bands 50 km wide
2 km x 2 km resolution & 8 mm accuracy
Synthetic Data produced by Gaultier et al. (2021) software
OSSE: Assimilation of SWOT SSH
Assimilation Sea Surface Salinity (SSS) from SMOS
SSS data was assimilated in a 4-d cycle in 2010 and 2012 into HYCOM 1/12
ASSIM 2010 - 2012
Assimilation could impose interannual variability
SSS Difference 2010 - 2012
T(oC) Difference With – Without PIRATA Jan-May 2012
OSE with PIRATA
Maps of time correlation of SLA (m) and AVISO for the Control Run, RODAS_EnOI and RODAS_EnKF
HYCOM+RODAS version with EnKF
RODAS_EnKF with only 11 members;
Trial period 01/06/2017 a 31/12/2017
Source: D.Sc. Thesis by Filipe Bitencourt Costa (Jul/2021)
Final Considerations
- BRICS to work with assimilation of data in the deep ocean and learn how to assimilate sea ice
- GOOS-BR to perform OSEs and OSSEs