Site selection for OWL using past, present, and future climate information

Selection of an ideal site for the new generation of Overwhelmingly Large (OWL) telescopes is dependent on many climatological and meteorological parameters. Among these are cloud cover, atmospheric humidity, aerosol content, air temperature, airflow direction, strength and turbulence. Even relatively minor changes in weather patterns can have a significant effect on seeing conditions. A composite climatological database has been designed and built for the site selection task at the Department of Geosciences, University of Fribourg, Switzerland. The database is mainly composed of ECMWF and NCEP-NCAR reanalysis data at a global resolution of between 1° and 2.5° latitude / longitude. Using a Java based interface, codenamed "FriOWL", and programmed in the style of a Geographical Information System, all of this relevant information can be interrogated in order to find the best possible sites for the new telescope. Perhaps the most important variable in site selection is the interaction between air-flow and topography, as atmospheric turbulence greatly affects the image quality produced by the telescope. Global climate is changing and it will continue to do throughout the 21st century. Therefore, it is important to ascertain the effect of global warming on potential sites. An ideal site in today’s climate may not prove ideal within 20 to 50 years. It is therefore planned to update the database with future climate data, using output from global climate models. High resolution modeling of the critical parameters at preferred sites under future climates is also planned.

[1]  Marc S. Sarazin,et al.  The eye of the beholder: designing the OWL , 2003, SPIE Astronomical Telescopes + Instrumentation.

[2]  Philippe Dierickx,et al.  OWL CONCEPT OVERVIEW , 1999 .

[3]  Marc S. Sarazin,et al.  New tools for a global survey of potential sites for the future giant telescopes , 2003, SPIE Astronomical Telescopes + Instrumentation.

[4]  M. Rebetez Changes in daily and nightly day-to-day temperature variability during the twentieth century for two stations in Switzerland , 2001 .

[5]  J. Houghton,et al.  Climate change 2001 : the scientific basis , 2001 .

[6]  M. Beniston Climatic Change in Mountain Regions: A Review of Possible Impacts , 2003 .

[7]  René Laprise,et al.  A Semi-Implicit Semi-Lagrangian Regional Climate Model: The Canadian RCM , 1999 .

[8]  Philippe Dierickx,et al.  Progress of the OWL 100-m telescope conceptual design , 2000, Astronomical Telescopes + Instrumentation.

[9]  E. Kaas,et al.  Changes in the storm climate in the North Atlantic/European region as simulated by GCM time-slice experiments at high resolution , 2022 .

[10]  T. V. Ommen,et al.  Observed climate variability and change , 2002 .

[11]  Francois Rigaut,et al.  Future of filled aperture telescopes: is a 100-m feasible? , 1998, Astronomical Telescopes and Instrumentation.

[12]  Martin Beniston,et al.  Changes in the anomalies of extreme temperature anomalies in the 20th century at Swiss climatological stations located at different latitudes and altitudes , 2001 .

[13]  M. Collins,et al.  Projections of future climate change , 2002 .

[14]  Stéphane Goyette,et al.  Application of the Canadian regional climate model to the Laurentian great lakes region: Implementation of a lake model , 2000 .

[15]  M. Beniston,et al.  Perturbations to astronomical observations at the European Southern Observatory’s very large telescope site in Paranal, Chile: analyses of climatological causes , 2002 .

[16]  Roberto Gilmozzi,et al.  Proceedings of the Backaskog workshop on extremely large telescopes , 2000 .

[17]  John Theodore Houghton,et al.  Global Warming: The Complete Briefing , 1994 .

[18]  Martin Beniston,et al.  Application of a new wind gust parameterization: Multiscale case studies performed with the Canadian regional climate model , 2003 .

[19]  Xuebin Zhang,et al.  Characteristics of Daily and Extreme Temperatures over Canada , 2001 .

[20]  V. Swail,et al.  The link between wave height variability in the north Atlantic and the storm track activity in the last four decades , 2002 .

[21]  R. Reynolds,et al.  The NCEP/NCAR 40-Year Reanalysis Project , 1996, Renewable Energy.