22 May 2008

Presentation Niamey, AMMA-ENSEMBLES meeting

Submitted Abstract:

As a consequence of the severe drought that occurs from 1970 to 2000, forecasting rainfall over the Sahel at seasonal time scales became a priority regarding to impacts in terms of food, health and security managements since the 1970’s. Improving the prediction of the West African Monsoon (WAM) system and its impacts on health, water resources and food security is one of the main aims of the AMMA (African Monsoon Multidisciplinary Analysis) project. In parallel, within the European DEMETER and ENSEMBLES projects framework, a well-validated European coupled multi-model ensemble forecast system for reliable seasonal to interannual prediction has been developed, and maintained at ECMWF. Using the model forecasts performed in ENSEMBLES and DEMETER projects in order to highlight their performance and their reliability over West Africa appeared to be essential, from the first cross AMMA/ENSEMBLES meeting that took place in Bamako, Mali.

Within this framework, we propose to highlight the performance of the different models participating in the ENSEMBLES and DEMETER projects in capturing the mean features of the WAM, as well as of the multi-model hindcasts, during the rainy season (from July to September) over the [1991-2001] common period. Different reference observation data sets are used (CRU, GPCP, NCEP....) to validate the model forecasts. This task is achieved using common validation tools, namely typical indices and maps to determine the model biases (mean/variability) and determinist/probabilistic scores (Correlation/Brier/ROC) to highlight the forecasts performance. A perfect model approach is also used to determine the potential predictability (PP) of the main impact variables (this analysis provides an idea about the upper limit of forecasting probabilities).

Preliminary results highlight common precipitation biases as simulated by coarse resolution GCM used in climate studies, namely overestimation of rainfall over the high mountains (Ethiopia plateau) and underestimation over the low ones (Cameroon mounts, Senegal coast). These biases are relatively similar for both the mean and the variance. Other common (well-known) biases are depicted for relevant SST areas, namely a warm bias over the Gulf of Guinea and the Eastern Pacific region (ENSO). The rainfall potential predictability is relatively high over the Guinea Coast whereas it is relatively weak over the Sahel. Moreover, the model rainfall forecasts seem to be more skilful over the Guinea Coast and the tropical Atlantic Ocean than the Sahel.

Similarities and differences between DEMETER and ENSEMBLES hindcasts systems over sub-Saharan Africa will then be given in the conclusion. A discussion will also be done about the limiting selected common period (1991-2001). Namely, is 10 year model climate enough to have significant statistical results (mean, variance, etc) over the Sahel? Strategies and methods to improve the model forecast performance will then be highlighted as perspectives.

Presentation link:
caminade_morse_Niamey.ppt

Guideline (few comments slide by slide):
guideline_Niamey.ppt

16 May 2008

Validation ENSEMBLES/DEMETER v1.2

An updated version of the validation Atlas of DEMETER/ENSEMBLES seasonal forecast over Africa. ROCSS and Brier Scores have been added for rainfall and 2m temperature.
Few results are discussed:

Atlas_ENSEMBLES_DEMETER_Africa.v1.2.pdf

The figures have also been updated on the flickr site:
http://flickr.com/photos/25358757@N06/sets/72157605087475214/

02 May 2008

20th century Sahel rainfall variability as simulated by the ARPEGE AGCM and future changes

Here is a first paper draft concerning the links between SST/Tropospheric temperatures and the Sahelian drought for the ARPEGE-climat model, and an highlight concerning the IPCC simulations:

clim_dyn_paper_caminade_terray_2008.pdf

25 April 2008

DEMETER/ENSEMBLES Africa/Florida presentation

Few slides (ppt file) and results concerning DEMETER/ENSEMBLES seasonal forecast over Africa can be retrieved to this link:

Conference_florida_Andy.ppt

An update of the Africa report would be done soon......

14 April 2008

Validation ENSEMBLES/DEMETER v1.1

The validation figures are now sorted on the associated flickr web site, in an album:
http://flickr.com/photos/25358757@N06/sets/72157604532681799/
The labels are now included in the figures.

Word and pdf documents are also available here:
Atlas_ENSEMBLES_DEMETER_Africa.doc
Atlas_ENSEMBLES_DEMETER_Africa.pdf

Other analyses (ROC/Brier scores, SST analyses....) will be available soon and uploaded on flickr and my blog.
The full report (including both the figures, labels... summarizing the set-up of the simulations and the main results) is still in progress...

04 April 2008

Validation ENSEMBLES/DEMETER over Africa

This is a first validation atlas version of ENSEMBLES/DEMETER forecast over Africa.
The figures will be updated in real time (this is only a first release):

http://www.flickr.com/photos/25358757@N06/

The name of the figure is explicit (I hope)
They are not sorted at the moment....
A clean document would be available soon

Select the "Validation ENSEMBLES/DEMETER Africa v1" album to visualize all the figures in a single window.

A link and a slide show is available too at the page bottom

18 February 2008

"Climate type" analysis of DEMETER seasonal forecats

Here are few figures concerning the different DEMETER coupled models ability to capture observed features of seasonal forecasts over West Africa:




Fig1: Mean seasonal rainfall (JJAS 1980-2001) as simulated by the different coupled models used in DEMETER forecasts, compared to CMAP observations.



Fig2: Mean seasonal rainfall (JJAS 1980-2001) anomalies as simulated by the different coupled models used in DEMETER forecasts with respect to CMAP observations.


Fig3: Seasonal rainfall (JJAS 1980-2001) standard deviation as simulated by the different coupled models used in DEMETER forecasts, compared to CMAP observations.



Fig4: Seasonal rainfall (JJAS 1980-2001) standard deviation anomalies as simulated by the different coupled models used in DEMETER forecasts, with respect to CMAP observations.




Fig5: Seasonal rainfall (JJAS 1980-2001) spatial correlations between the different coupled models used in DEMETER forecasts, and CMAP observations.

Fig6: Seasonal rainfall (JJAS 1980-2001) potential predictability as simulated by the different coupled models used in DEMETER forecasts.



Fig6:
Sahelian rainfall index (JJAS 1980-2001, 16W-40E, 10N-20N) as simulated by the different coupled models used in DEMETER forecasts compared to CMAP observations (CMAP black line, Ensemble mean red line).