HIRLAM activities on the use of satellite data

Ad Stoffelen, KNMI


Several members of the HIRLAM group are conducting research and development on the assimilation of satellite data in the HIRLAM model and these are organised in a HIRLAM subproject. DNMI invited this group for a meeting on 6 November 1997 where the progress and plans in the area were discussed. Here follows a brief account of the activities.

SCATTEROMETER WORK

Status

At the meeting Harald Schyberg presented the work done at DNMI to utilise scatterometer data in the HIRLAM model. An error analysis method based on division of observation errors into physical and observation space is used to derive a general form of the observation error contribution to the cost function. The method is utilised operationally for ambiguous scatterometer wind observations at DNMI. Ad Stoffelen presented results from an experiment on the use of scatterometer data in the HIRLAM analysis/forecast system in a period where both ERS-1 and ERS-2 data were available. The results showed a positive scatterometer impact on the first guess in all experiments, and on the forecasts when data from both satellites were used, but insignificant forecast impact with data from only one satellite. With the increased data coverage from the NASA QuikSCAT (1998 launch), ADEOS-II SeaWinds (2000), and METOP ASCAT (2003) this is promising.

Plans

KNMI will develop and implement the scatterometer sea surface wind product of the EUMETSAT Ocean & Sea Ice SAF, and be responsible for pre-processing, bias tuning etc. In 1998 ambiguous wind vectors will become available through the SAF. It was agreed that the processing system (PRESCAT) and assimilation system for scatterometer data in OI at KNMI should be made operational and a part of the HIRLAM reference system. KNMI will also work on the use of scatterometer data from other satellites such as the planned NASA QuikSCAT and ADEOS-II SeaWinds. QuikSCAT will be on a dedicated polar orbitter and planned for real-time delivery at the beginning of 1999. It has a 1800 km broad swath. QuikSCAT bridges a gap between ERS-2 and ASCAT. Due to its scanning geometry, research and development is required in order to achieve an appropriate data assimilation. As 3dvar becomes available in HIRLAM, DNMI will implement variational analysis of ERS scatterometer winds based on their operational version of the cost function in 1998.

NWP SAF

Ad Stoffelen presented the status and plans for the NWP SAF where KNMI plans to be a partner together with the U.K. Met. Office, ECMWF and Meteo France. The SAF will co-ordinate the interface between satellite data processing and data assimilation. It was agreed that the SAF will be a useful tool for the HIRLAM group as the results will be available for all EUMETSAT member states. In 1998 Ad Stoffelen will make an inventory of the HIRLAM requirements and priorities as input to the NWP SAF work programme.

(A) TOVS work and plans.

There has been a problem in accomplishing the work at FMI as key-persons have left FMI this year. However, Niko Sokka started in August, and he presented the status of the TOVS work at FMI. 1D-var is implemented and tested in the HIRLAM analysis with neutral impact. Work is ongoing with cloud clearing, bias correction and better utilisation of the locally received data on 40 km resolution. In the HIRLAM group FMI can usefully contribute with their experience on 1D-var and with work on bias correction and impact studies. At SMHI Per Unden started working on the utilisation of TOVS data. The work will be both on 1D-var and 3D-var, and, as SMHI is responsible for the high latitude part of the nowcasting SAF, on cloud clearing problems. DNMI started a 4-year project on the use of ATOVS. DNMI will especially look into the observation error statistics and the problems of utilising the data at high resolution. As DNMI has responsibilities for sea ice and SST in the Ocean & Sea Ice SAF it will also be natural to focus on the effects of ocean and ice surfaces. KNMI is working on the implementation of the processing package AAPP, and also assisted other HIRLAM members (DNMI) with this. The expected extensions of AAPP (e.g., 1D-var) will also be implemented by KNMI.

(B) Other Satellite data

KNMI and Meteo France participate in the EU SODA project on assimilation of ozone data. The work is on extraction of dynamic information around the tropopause from the data, and on effects from ozone on the radiative transfer model. The HIRLAM project awaits the success of this approach. SMHI starts a project on 4D-var assimilation of ground-based GPS. In the Nordic countries there are 50 stations working with 5 minutes time resolution giving possibilities for indirect moisture observations. It was agreed that this should be brought into the HIRLAM plans. Co-ordination should be considered with GPS activities at DMI and KNMI.