1. Observations of foehn interaction with lake breeze and valley wind circulations, Lake Tekapo, New Zealand Hamish McGowan School of Geography, Planning and Architecture, University of Queensland, Brisbane, Australia

2. Research collaborators Prof. Andy Sturman Centre for Atmospheric Research, University of Canterbury, Christchurch, NZ Dr. Meinolf Kossmann German Meteorological Service (DWD), Offenbach a. M., Germany Dr. Peyman Zawar-Reza Centre for Atmospheric Research, University of Canterbury, Christchurch, NZ

3. Aim Of The Research To develop a clearer understanding of the interaction of thermal and dynamic forcing of airflow in complex terrain. Improve knowledge of the way in which various atmospheric processes interact in particularly complex environments to develop equally complex local wind regimes.

4. Background 6 years of complex terrain windfield research – foehn triggered dust storms. Frequent observation of foehn events that were not forecast (potential wind hazard). Increased development of New Zealand’s alpine region (tourism, agriculture) requiring improved local and meso-scale forecasting capabilities

5. South Island of New Zealand Source NASA

6. Lake Tekapo study area (April 1998) Source NASA

7. Looking north over Lake Tekapo

8. View south over Lake Tekapo

9. Godley Valley

10. The upper Godley Valley and Main Divide

11. Meteorological Monitoring Network 1997 - 1999

12. ‘Typical’ foehn Moderate to strong foehn nor’wester dominates regional windfield Wind speeds in alpine valleys may > 40 ms -1 Significant orographic rainfall and spillover precipitation Barrier jet formation upwind of barrier with well developed lee trough formation downwind

13. 14 February 1999 Alpine foehn not forecast! Rawinsonde soundings identified ridge-top (2500 m agl.) light W/NW gradient flow at 5ms -1 Thermally driven circulations recorded at most coastal and lowland locations Foehn onset recoded in the Godley Valley at 1000NZST – linked to local surface heating

14. Foehn advance and retreat, 14 Feb 1999

15. Vertical wind speed and direction profiles – Godley Valley 1600

16. Foehn – Lake Breeze Interaction Typical light foehn – lake breeze interaction (a). Cold air ramping (an important mechanism for pollution dispersion). 14 February 1999 situation (b). May result in fumigation over lake and associated shoreline Foehn Valley wind (a) (b) Valley wind

17. Conclusions The wind field at Lake Tekapo represents a complex superposition of multi- scale wind systems: Ülake/land breezes, up-/down-slope winds, mountain/valley winds, plain- to-basin circulation and foehn Foehn onset ‘initially’ governed by airflow at 500hPa, surface sensible heat flux, thermally induced local and regional scale circulations. During light/moderate foehn conditions the topographically channelled foehn regularly decouples from the surface and flows over the lake breeze (cold air ramping). The foehn may ground over the downwind shoreline in response to increased surface mixing (fumigation possible) A climatology of alpine foehn events is to be developed (ie to improve forecasting of alpine foehn, role of foehn in mean annual temps)