81. UV Index (UVI) Map: World, US, Australia, New Zealand. UV Intensity. SafeSun UV Updated daily. From SafeSun.Category News Weather UV Index...... level must take into account information on the time, date, latitude, cloud, altitude,haze and ozone concentrations. The Bureau of meteorology worked with the http://www.safesun.com/uv_map.html

UV Intensity maps SafeSun , Personal UV meter measures UV intensity in UV Index (UVI) units. UV maps may load slowly. At times, some maps will be unavailable. They are all taken from remote servers. Updated daily. UVI world map Because of problems with TOMS, the freshest is from Dec 31, 2000 This map is provided courtesy of the Socioeconomic Data and Applications Center ( SEDAC The Center for International Earth Science Information Network ( CIESIN ) at Columbia University has been designated by NASA to operate and maintain SEDAC. Data Description: This map represents local noon near-real time estimates of the UV Index (UVI) using total column ozone abundances measured by NASA's Total Ozone Mapping Spectrometer (TOMS) carried by the Earth Probe satellite. Cloud cover is not incorporated. TOMS news UVI US map This map is provided courtesy of the National Oceanic and Atmospheric Administration ( NOAA ) and the Environmental Protection Agency ( EPA Data Description: Australia UVI forecast This map is provided courtesy of the Commonwealth Bureau of Meteorology , Australia.

82. Cooperative Research Centres (CRC) - Southern Hemisphere Meteorology This Centre is a major worldclass centre for meteorology research and graduatetraining, with three research programs ozone; Transport Modelling; and http://www.crc.gov.au/centres/Old_CRCs/shm.htm

Melbourne (VIC) Sydney (NSW) Core Participants: Industry: Silicon Graphics Pty Ltd. University: Monash University. Commonwealth: Bureau of Meteorology; CSIRO, Atmospheric Research. Research Focus Areas of Research Expertise Dynamical meteorology, atmospheric chemistry and physics, numerical weather and climate modelling, atmospheric general circulation, stratospheric dynamics, data analysis and inverse methods. Centre Established: 1 July 1993 Round No: Grant Period: 7 Years I ncorporated: No Personnel involved in Centre Postgraduate students 31 Full-time equivalent research staff 27 Funding 1999/00 dollars ($ million) Average Funding per annum Total Funding over Grant period CRC Program Funding Total Resources for Centre Contact Details Chair: Professor John M Swan Professor David Karoly Director CRC for Southern Hemisphere Meteorology 3rd Floor, Building 70 Monash University Wellington Road CLAYTON VIC 3168 Tel: (03) 9905 9669 Fax: (03) 9905 9689 E-mail: crc@vortex.shm.monash.edu.au

83. Meteorology Copyright ©1998 The McGrawHill Companies. All rights reserved. Any use is subject to the Terms of Use and Privacy Policy. For further information about this site contact mhhe_webmaster@mcgraw-hill.com. http://www.mhhe.com/earthsci/geology/danielson

and For further information about this site contact mhhe_webmaster@mcgraw-hill.com . McGraw-Hill Higher Education is one of the many fine businesses of The McGraw-Hill Companies

84. Uncoupling Meteorology From Ozone--One Approach Uncoupling meteorology from OzoneOne Approach. Classify days by meteorologicalconditionstemperature, wind speed, wind direction (binning). http://www.ladco.org/monitor/ozone_trends/tsld003.htm

Uncoupling Meteorology from OzoneOne Approach Classify days by meteorological conditionstemperature, wind speed, wind direction (binning) Focus on ozone conducive conditions Log-transform data (comes closer to normality, and trends can be interpreted as % change/year) Examine trends on similar days by regression Limit analysis to single day episodes and first day of multi-day episodes Previous slide Next slide Back to first slide View graphic version

85. Uncoupling Meteorology From Ozone--One Approach First Previous Next Last Index Home Text. Slide 3 of 34. http://www.ladco.org/monitor/ozone_trends/sld003.htm

86. CABO - Climate And Background Ozone Research Group by the British Council (London) to start in 1991 - her research on meteorologyand ozone under the supervision of Professor Trevor D. Davies, Professor http://www.giub.unibe.ch/~evi/cabo/

CABO - Climate and Background Ozone Research Group Swiss-British Collaboration Jungfraujoch Studies TROTREP ACCORD ... Publications Oldies Evi on 'Graduation Day', 1995 at UEA, together with Professor Stuart A. Penkett (UEA-ENV, Norwich, U.K.) CABO trip to the Swiss Meteorological Institute at Locarno-Monti, autumn 1996 News MOWIS - Mentoring Of Women In Science - a pilot project at Berne University in the framework of LEONARDO DA VINCI Zanis, P., P.S. Monks, E. Schuepbach, L.J. Carpenter, T.J. Green, G.P. Mills, S. Bauguitte, and S.A. Penkett, 2000: In-situ ozone production rate and the ozone compensation point during FREETEX '98 at the Jungfraujoch in the Swiss Alps. J. Geophys. Res. 105(D19), 24,223-24,234. Carpenter L.J., T. Green, G. Mills, S. Bauguitte, S.A. Penkett, P. Zanis, E. Schuepbach, N. Schmidbauer, P.S. Monks, C. Zellweger, 2000: Oxidised nitrogen and ozone production efficiencies in the springtime free troposphere over the Alps. J. Geophys. Res., 105(D11), 14,547-14,559. Broennimann S., E. Schuepbach, P. Zanis, B. Buchmann, and H. Wanner, 2000: A climatology of regional background ozone at different elevations in Switzerland (1992-1998).

87. References Bloomfield, P., Royle, A. and Yang, Q. (1993). Rural ozone and meteorologyanalysis and comparison with urban ozone. Technical http://www.cgd.ucar.edu/stats/web.book/BOOK/node12.html

Next: Online datasets and software Up: Modeling Ozone in the Previous: Overview of the Case References Bates, D.M. and Watts, D.G. (1988). Nonlinear Regression Analysis and its Applications . Wiley, New York. Becker, R.A., Chambers, J.M. and Wilks, A.R. (1988). The New S Language: A Programming Environment for Data Analysis and Graphics. Wadsworth and Brooks/Cole, Pacific Grove, CA. Bloomfield, P., Royle, A. and Yang, Q. (1993). Rural ozone and meteorology: analysis and comparison with urban ozone. Technical Report 5. National Institute of Statistical Sciences, Research Triangle Park, NC. Bloomfield, P., Royle, A., Steinberg, L.J. and Yang, Q. (1996). Accounting for meteorological effects in measuring urban ozone levels and trends. Atmospheric Environment Chambers, J.M. and Hastie, T.J. (eds.) (1993). Statistical Models in S Cox, W. M. and Chu, S.-H. (1993). Meteorologically adjusted ozone trends in urban areas: A probabilistic approach. Atmospheric Environment Davison, A.C. and Smith, R.L. (1990). Models for exceedances over high thresholds (with discussion). Journal of the Royal Statistical Society, series B

88. The East Tennessee Ozone Study (ETOS) A case in point is shown. The day in question was one of ozone exceedance. Onsitemeteorology would have said that the origin lay to the southwest. http://www.arl.noaa.gov/milestn/mile4.html

The East Tennessee Ozone Study (ETOS) Phase 1 of the Appalachian Highland Ozone Exceedance Prediction Program The summer of 1998 produced alarming headlines in Knoxville papers. The Knoxville News Sentinel reported that "Air Quality at Clingman's Dome Reaches Danger Level" and "Smoky's Air Quality Setting Worst Records." During the summer of 1998, air monitoring stations in the Great Smoky Mountains National Park recorded the highest-ever eight-hour average ozone exposures. By late August, the National Park Service reported the 25 th day of unhealthy ozone conditions for 1998. The problem: High altitude regions of the Appalachians, from Georgia to New York, are increasingly affected by ozone exceedances. We risk losing access to the Appalachian National parks and other elevated areas, for asthmatics and others with breathing disorders. Moreover, sensitive components of the ecosystem are increasingly affected. Access to parks might be limited on occasions when extremely high concentrations of ozone are expected. Data from Cove Mountain in Tennessee illustrate the problem. The figures shown (for July and August 1995) are not selected to show anything unusual. Rather, they show what is expected to be a typical wind direction dependence for occasions with high ozone concentrations.

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