1. An attempt to homogeneously describe 60 years statistics of TC activity in E Asia, 1948-2007
Hans von Storch and Frauke Feser
1Institute for Coastal Research, GKSS Research Center, Germany
2clisap-Klimacampus, University of Hamburg, Germany
45 min‘s
· Ideally a review of the methods employed in your field to detect and analyze change and feedbacks, finishing off with what the state of the art is in the methods and suggestions for newer methods that might be transferable to hydrologic extremes
· We are most interested in the methods you employ rather than a possible synthesis with hydrology
· Summarize the challenges you are facing detecting and analyzing change and feedbacks and assigning causality to them

2. Applications: past and future marine weather in N Europe
downscaling cascade for constructing variable regional and local marine weather statistics
Simulation with barotropic model of North Sea
Globale development (NCEP)
45 min‘s
· Ideally a review of the methods employed in your field to detect and analyze change and feedbacks, finishing off with what the state of the art is in the methods and suggestions for newer methods that might be transferable to hydrologic extremes
· We are most interested in the methods you employ rather than a possible synthesis with hydrology
· Summarize the challenges you are facing detecting and analyzing change and feedbacks and assigning causality to them
Dynamical Downscaling REMO or CLM
Cooperation with a variety of governmental agencies and with a number of private companies

3. Baroclinic storms in N Europe
Problem for synoptic systems solved by in N Europe, using RCM spectrally nudged to NCEP
retrospective analysis
good skill with respect to statistics, but not all details are recovered.
45 min‘s
· Ideally a review of the methods employed in your field to detect and analyze change and feedbacks, finishing off with what the state of the art is in the methods and suggestions for newer methods that might be transferable to hydrologic extremes
· We are most interested in the methods you employ rather than a possible synthesis with hydrology
· Summarize the challenges you are facing detecting and analyzing change and feedbacks and assigning causality to them
Weisse, R., H. von Storch and F. Feser, 2005: Northeast Atlantic and North Sea storminess as simulated by a regional climate model and comparison with observations. J. Climate 18,

4. Downscaling SE Asian marine weather
We have implemented the dynamical downscaling approach for SE Asian marine weather.
The key question is – will we master the description of typhoons?
Done: Case studies and seasons – formation of typhoons induced by large scale dynamics and NOT by initial values.
Presently under examination: Continuous 6-decade simulations constrained by NCEP global re-analyses.
Feser, F.,and H. von Storch, 2008: Regional modelling of the western Pacific typhoon season 2004, Meteor. Z. 17 (3), DOI: / /2008/0282
Feser, F., and H. von Storch, 2008: A dynamical downscaling case study for typhoons in SE Asia using a regional climate model. Mon. Wea. Rev. 136,
45 min‘s
· Ideally a review of the methods employed in your field to detect and analyze change and feedbacks, finishing off with what the state of the art is in the methods and suggestions for newer methods that might be transferable to hydrologic extremes
· We are most interested in the methods you employ rather than a possible synthesis with hydrology
· Summarize the challenges you are facing detecting and analyzing change and feedbacks and assigning causality to them

5. A case study: Simulating tropical storm Winnie (August 1997) with regional atmospheric model CLM
45 min‘s
· Ideally a review of the methods employed in your field to detect and analyze change and feedbacks, finishing off with what the state of the art is in the methods and suggestions for newer methods that might be transferable to hydrologic extremes
· We are most interested in the methods you employ rather than a possible synthesis with hydrology
· Summarize the challenges you are facing detecting and analyzing change and feedbacks and assigning causality to them

6. 12 TCs in Season 2004 only 10 were found in CLM simulation
Following Zhang et al., Meteor. Atmos. Phys.

8. Complete simulation of 1948-2007 using CLM with 0
Complete simulation of using CLM with 0.5º grid resolution and NCEP/NCAR reanalysis
Spectral nudging of scales larges than about 800 km.
Results are new; thus may be subject to future revisions!

9. Criteria have subjectively been selected so that the mean number of TCs detected in the simulation is about equal to the mean number given in the best track data.

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12. Conclusions
(Some) typhoons can be described by regional atmospheric models run in the climate mode.
But, downscaled (simulated) TCs are too weak in terms of core pressure, maximum pressure fall and maximum sustained wind.
We need better data for validation.
Preliminary results concerning change
Strong year-to-year variability
Little decadal variability
No overall trend in numbers
Slight upward trends in minimum pressure and max wind since 1990s.

13. Next workshop: 11+12 March 2009, Taipei or Tainan, Taiwan