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         Ozone Meteorology:     more books (100)
  1. Measurements of atmospheric ozone at Resolute, Canada (74 ̊43ʺN; 94 ̊59ʺW): July 7, 1957 to December 31, 1959 (Canada. Meteorological Branch. Canadian meteorological memoirs) by H. M Sullivan, 1961
  2. Atmospheric ozone investigations at Barrow, Alaska, during 1965 by John Joseph Kelley, 1967
  3. Observations of the total amount of atmospheric ozone at Uppsala, Sweden, from 1951 to 1966 (Report - Dept. of Meteorology, University of Uppsala) by Sven Birger Rindert, 1975
  4. Trends in carbon monoxide and ozone concentrations in Southeast Michigan, and the influence of meteorology (A technical report / Southeast Michigan Council of Governments) by David Derenzo, 1981
  5. The winds of Colorado ; Ozone observations by Charles Denison, 1876
  6. A Composite study of cloud, ozone and other data from recent satellite experiments (GSFC) by M. S. V Rao, 1973
  7. Ozone measurement system for NASA Global Air Sampling Program (NASA technical paper) by Marvin W Tiefermann, 1979
  8. The meteorology of Clifton, being the results of ten years' observations of the barometer, thermometer, rain, &c, &c., recorded at no. 7, South Parade, Clifton, Bristol by William C Burder, 1863
  9. Ozone Correlative Measurements Workshop proceedings of a workshop (SuDoc NAS 1.55:2362) by NASA, 1985
  10. Development of a meteorological index for the assessment of ozone trends by Terry A Sweitzer, 1986
  11. Distribution of total ozone content of atmosphere according to satellite observations (JPRS) by V. M Berezin, 1973
  12. Chemistry and Physics of Stratospheric Ozone, Volume 74 (International Geophysics) by Andrew Dessler, 2000-07-10
  13. Ozone and Climate Change: A Beginner's Guide by Stephen J. Reid, 2000-02-01
  14. Stratospheric Ozone Depletion/UV-B Radiation in the Biosphere (NATO ASI Series / Global Environmental Change)

61. Ph.D Studentships Are Available Each Year For NERC-eligible Students. Other Stud
The meteorology Group has a longstanding collaboration with a team at NASA'sJet of key chemical species in the atmosphere, such as ozone, water vapour
http://www.met.ed.ac.uk/~kjw/phds.shtml
Ph.D studentships are available each year for NERC-eligible students. Other students must secure an alternative source of financial support. A specific topic for study should be agreed in consultation with staff but the list below is typical: Applicants for NERC studentships should check that they satisfy NERC eligibility requirements. An on-line application form can be found here Daily cycles in Earth radiation balance. Supervisor: Dr Chris Merchant. Clouds affect the solar energy entering (warming) the climate system and the energy radiated to space by Earth (cooling). Their net effect is therefore a balance between warming and cooling effects. Since the balance depends on many factors that may change in the future, the largest single uncertainty in the sensitivity of climate to human perturbations of CO2 is the role that clouds will play. The mean change in radiation balance due to clouds depends on the timing of the cloud properties relative to solar illumination and the daily temperature changes of the surface. Many cloud types have daily cycles in their properties, but this has not been fully investigated largely for lack of suitable observations. New satellite-based observations (Meteosat Second Generation) over the European-African hemisphere will be available from this year (2003) with several aspects uniquely suited to investigating further and relating observed cycles of radiation balance to models of clouds in the climate system. Contribution of tropical cyclones to air-sea fluxes of CO2. Supervisor: Dr Chris Merchant

62. OMI-URD: Operational Meteorology Requirements
Table 3.2 Threshold user requirements for operational meteorology. Total ozone,A, 1, better than IASI, 250 × 250, 125 × 125, n/a, 3, NWP; analysis of UV
http://www.knmi.nl/onderzk/atmosam/omi/node4.html
Next: Climate Monitoring Requirements Up: OMI-URD Previous: OMI Mission Objectives
Subsections
3 Operational Meteorology Requirements
As indicated earlier the OMI mission objectives in the area of operational meteorology are envisaged to comprise the provision of data to improve Numerical Weather Prediction (NWP), the analysis of ultraviolet radiation levels and the monitoring and prediction of the evolution of volcanic clouds. The operational meteorological application differs from other applications of OMI data in several ways:
a)
The timely delivery of the data is essential. If the data are not delivered in time the observations soon loose their value.
b)
These data will be assimilated completely automatically as large amounts of data are involved (though there is quality control through computer generation of data quality and error statistics).
c)
Subtle trends in the data caused by ageing of the equipment are not a major concern for numerical weather forecasting.
At this moment it is still unclear whether it will be better to assimilate retrieved products (i.e. ozone profiles and columns, columns of other trace gases and aerosols, etc.) or the observed radiances directly into the weather forecast models. This question will have to be addressed in the coming years. In the following discussion it is assumed that retrieved products will be used.

63. FSU Department Of Meteorology
Center for OceanAtmospheric Prediction Studies) trains scientists in Meteorologyand Physical the oxidizing power of the atmosphere including ozone, H2O, NO
http://www.met.fsu.edu/research/
DEPARTMENTAL RESEARCH
COAPS
Headed by Distinguished Professor of Meteorology and Oceanography James O'Brien, COAPS (the Center for Ocean-Atmospheric Prediction Studies) trains scientists in Meteorology and Physical Oceanography. COAPS is the focus at the Florida State University for research in interannual and interdecadal variability of the Earth's climate affected by the tropical and mid-latitude oceans. COAPS is funded by several federal agencies to produce original and published papers that advance understanding of the ocean and atmosphere. In recent years, COAPS has been internationall recognized for its studies on the impact of El Nino on severe weather.
COMET
To meet the objective of improving mesoscale forecasting in the United States, an Outreach Program was developed at the COMET Program. This program currently provides financial support to universities for collaborative research projects, graduate student fellowships, postdoctoral fellowships, and other activities.
LBA
he purpose of this homepage is to provide the LBA-Ecology Science Teams a means to monitor the GOES 8 imager data that are being archived for the LBA-Ecology Project. A 24-hour rotary archive of real-time Imager Channel 1-5 pictures, presented in JPEG format, are provided to show the general meteorological conditions. A full catalog of the archived datasets (i.e., day-time IDs) is also available.
PEM-TROPICS
The two major objectives of PEM-Tropics are:
1.To provide baseline data over the Basin for gases important in controlling the oxidizing power of the atmosphere including ozone, H2O, NO, CO, and NMHC's;

64. Resources For Teaching Meteorology
air pollution; ozone Depletion Information from the EPA; Air PollutionEPA resources on air quality and pollution; NOAA National
http://www.csun.edu/~vceed002/geoscience/meteorology/
Chapters: Sourcebook for Teaching Science (1) Thinking Scientifically (2) The Science Curriculum (3) The Language of Science (4) Communicating Concepts (5) Problem Solving in Science (6) Science Activities and Projects (7) The Science Laboratory (8) Professional Issues Internet Resources for Teaching Science Resources for Teaching Biology Resources for Teaching Chemistry Resources for Teaching Physics Resources for Teaching Geoscience Resources for Teaching Health Lesson Development Science Laboratory Professional Development Science Education at CSUN Teaching Resources
  • The Weather Channel: Automated Weather Source : Worldwide weather and teaching resources The Aurora Page : Information on the Northern Lights
  • The Atmosphere
  • Current Air Pollution Readings : National readings on air pollution Ozone Depletion : Information from the EPA Air Pollution : EPA resources on air quality and pollution NOAA : National Oceanic and Atmospheric Administration Climatic Monitoring Laboratory : Monitoring of greenhouse gases, aerosols, ozone, etc.)
  • 65. Cun-kisuiken
    Polar meteorology and Glaciology No.13(1999). Influences of Arctic ozone hole onthe stratospheric general circulation Toshihiko Hirooka, Toshihiko Nishiyoshi
    http://www.nipr.ac.jp/library/m-gl.html
    Polar Meteorology and Glaciology, ISSN 1334-3437
    Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, ISSN 0914-2037
    CONTENTS
    Polar Meteorology and Glaciology No.16(2002)
    Polar Meteorology and Glaciology No.15(2001)
    Polar Meteorology and Glaciology No.14(2000)
    Polar Meteorology and Glaciology No.13(1999)
    Polar Meteorology and Glaciology No.16(2002) Satellite observation of melting and break-up of fast ice in Lutzow-Holm Bay, East Antarctica
    Hiroyuki Enomoto, Fumihiko Nishio, Hideo Warashina and Shuki Ushio cc1 Sea ice thickness estimated from passive microwave radiometers
    Kazutaka Tateyama, Hiroyuki Enomoto, Takenobu Toyota and Shotaro Uto cc15 Impact of satellite gravity missions on glaciology and Antarctic Earth sciences
    Yoichi Fukuda, Shigeru Aoki and Koichiro Doi cc32 Ice-flow characteristics over a rough bedrock: implications for ice-core interpretation
    Frank Pattyn cc42 Formation processes of a pocket consisting of bubble-free ice in Hamna ice cliff, Soya Coast, East Antarctica
    Yoshinori Iizuka, Hiroshi Satake and Okitsugu Watanabe cc53

    66. Ozone Weekend Effect
    When meteorology is not favourable for ozone prodution, weekends showgenerally higher ozone peaks than weekdays. Favourable meteorology
    http://sinus.unibe.ch/~broenn/week.htm
    Atmospheric Environment , Vol. 31 (1997), 1127-1135.
    Weekend-weekday differences of near-surface ozone concentrations for different meteorological conditions
    Stefan Brönnimann and Urs Neu Institute of Geography, University of Bern, Hallerstr. 12, 3012 Bern, Switzerland
    Back to Stefan Brönnimann's home page
    Climatology and Meteorology Research Group University of Bern
    stefanb@lpl.arizona.edu

    67. Environmental Programs Photochemical Model Ozone Forecasting
    visualize the crossboundary issues. ozone forecasts consistent withMM5 forecast meteorology. improved forecaster understanding of the
    http://www.emc.mcnc.org/services/realtime/
    Environmental Programs
    Real-time Photochemical Model Forecasting Service for States/Agencies
    Table of Contents
    I. Introduction II. What is Photochemical Model Forecasting? III. Forecast Products You Will Receive IV. Benefits to Your Forecast Process and Modeling Program ... IX. How to Sign Up
    I. Introduction
    Beginning in 1998, MCNC began to produce photochemical model forecasts of tropospheric ozone, precursors, and wet/dry deposition. To do this, we implemented MAQSIP-RT in real-time, which uses an enhanced version of the Carbon Bond-4 chemical mechanism. MAQSIP-RT is a close cousin of EPA's Models-3/CMAQ. The program was begun without formal funding, but in 1999 the Texas Natural Resource Conservation Commission (TNRCC) invested in developing the forecast system over Texas, and that program continued in 2000. Now, in 2001, the North Carolina Department of Environment and Natural Resources (NC-DENR), along with the city of Birmingham, Alabama, have joined with TNRCC as funding partners. Evaluations of the forecast performance of the model for the NE US (1998) and for Houston/ Galveston (2000) have shown that the model is a useful tool to assist day-to-day ozone forecasting on both regional and urban scales. This can be particularly advantageous for states that have multiple forecast zones, because it is increasingly difficult to develop and maintain many individual statistical/heuristic approaches, each one zone-specific.

    68. Project Atmosphere Australia On-line Weather Topic - Ozone Depletion
    Above the release of the ozonesonde balloon from the Bureau of meteorology TrainingCentre Field Annexe into cloudy skies on a gloomy, cold day in Melbourne.
    http://www.schools.ash.org.au/paa1/ozone.htm
    Online weather activities for schools conducted in a spirit of friendship and cooperation...
    Hosted from Elimbah - Queensland, Australia. Take a virtual tour! Home Description Instructions ... Links
    Teacher Support Teacher Training Net Meetings Weather Questions Activity Answers BOM/PAA Resources Resource Downloads Weather Stations Virtual Travellers Cognitive Processes Earth Systems Units Instrument Reviews Poetry Writing Inland Explorers Tropical Storms Weather Instruments Experts On-line PAAO Project Board Recording, Comparing Investigating a Region Trip Planning Activity Weather Partners Classroom Activities Activities Introduction Weather Puzzles Discovery Activities Weather Questions Weather Instruments Weather Art Weather Writing Weather Photos Weather Animations Weather Data Making Web Pages Match the Forecasts Logo Design Inland Explorers Virtual Field Trips Weather Journeys Weather Songs Online Activities Introductions Partner Classes Weather Travellers Weather Sharing Ask an Expert Weather Folklore Weather Writing Weather Reports Weather Prediction Weather Jokes Follow Journeys Weather Topics Ozone Depletion Snow The Atmosphere Weather Folklore Coriolis Effect Weather Photography Fog Rain and Hail Seasons:Arnhem Land Weather Jokes Weather Careers Soon! Wind

    69. NERC Grants On The Web
    meteorology. NERC Reference GST032466. Period of Award 1.10.1999 30.9.2003.Award Type Thematic, Upper Troposphere Lower Stratosphere (UTLS) ozone (ozone).
    http://gotw.nerc.ac.uk/grantlist_inst_med.asp?pi=2994&atype=

    70. Max Planck Institute For Meteorology
    Figure 1 below shows ozone volume mixing ratios from the surface up to about 250km computed by the recently developed HAMburg MOdel of the Neutral and Ionized
    http://www.mpimet.mpg.de/en/depts/bgcs/
    Home Staff Organisation Science ... Library Biogeochemical System Department
    Head Prof. Dr. Guy Brasseur
    Contact
    Dr. Hans Graf
    Sekretary Elke Lord
    phone.: +49-40-41173-421
    fax: +49-40-41173-430
    Scientific Working Groups
    Atmospheric Chemistry (Dr. Martin Schultz)
    Atmospheric Aerosol
    (Dr. Johann Feichter)
    Biogeochemical Cycles
    (Dr. Claire Granier)
    Ocean Biogeochemistry
    (Dr. Ernst Maier-Reimer)
    Middle and Upper Atmosphere Modelling
    (Dr. Marco Giorgetta)
    Analaysis and Process Modelling
    (Dr. Hans Graf) Director's Research Group (Prof. Dr. Guy Brasseur)
    Recent Results
    Figure 1 below shows ozone volume mixing ratios from the surface up to about 250 km computed by the recently developed HAM burg MO del of the N eutral and I onized A tmosphere (HAMMONIA). The model has been designed to study interactions between chemistry, dynamics and radiation in the mesosphere and lower thermosphere region and to investigate the coupling between the atmospheric layers. The zonal mean plot exhibits clearly three ozone maxima, the stratospheric one, the secondary in the mesopause region, and the recently discovered tertiary maximum at about 70 km height near the polar night terminator (Marsh et al., GRL, 2001). Fig. 1: Zonal mean ozone volume mixing ratio for summer solstice conditions

    71. MP: Ozone And Atmospheric Physics
    ozone Depletion US Environmental Protection Agency. Chemistry A; EGS AtmosphericPhysics and Chemistry; Tellus - Series B Chemical and physical meteorology.
    http://www-atm.physics.ox.ac.uk/user/markp/ozoneatmphys.html
    Information on Ozone and Atmospheric Physics

    Ozone Organizations Information
    Organizations International
    • World Meteorological Organization - WMO Stratospheric Processes And their Role in Climate - SPARC International Global Atmospheric Chemistry - IGAC
    UK
    Europe
    North America
    Journals AGU
    Online journals from Science Direct

    72. S. Trivikrama Rao
    meteorology on ambient ozone concentrations, 1997. Daniel Chan Linkingchanges in ozone to changes in meteorology and emissions, 1998.
    http://www.atmos.albany.edu/facstaff/rao.html
    S. Trivikrama Rao Research Professor, Environmental Sciences Office: 50 Wolf Road - Room 198 Phone: (518) 457-3200; Fax: (518) 485-8410; E-Mail: strao@dec.state.ny.us
    M.Sc. (Tech.) (Geophysics), 1965, Andhra University, India
    Ph.D. (Atmospheric Science), 1973, State University of New York at Albany Research Interest: Biogenic and anthropogenic sources of emissions are responsible for air pollution problems such as ozone, fine particulate matter, acid rain, visibility impairment, etc. Once released into the atmosphere, some pollutants are transported long distances by the prevailing winds, contributing to air pollution problems on a regional-scale. The entire process of atmospheric transport, transformation, diffusion and deposition must be fully understood to quantitatively examine the source-receptor relationships for air contaminants. The models are being used to examine the cause and effect relationships, and to identify strategies for controlling air pollution. Our current research is aimed at developing methods for evaluating air quality models and integrating observations and modeling results to examine the effectiveness of environmental management strategies. We are also developing and applying statistical methods for the analysis and interpretation of complex environmental data sets. Our research involves computer simulation modeling and applications of statistical techniques for studying air pollution problems. We are conducting collaborative research involving faculty at the University of Athens in Greece, University of Idaho, Cornell University, Harvard University, Rutgers University, Pennsylvania State University, University of Maryland, Columbia University, and with scientists at several State and Federal agencies in the U.S. and Canada.

    73. Essays And Essays Writing Essays On Meteorology - 195-003
    Papers On meteorology Page 4 of 5. ozone Layer Depletion send me this essay A6 page paper defining the ozone layer, its importance to life on Earth and the
    http://essaypage.com/categories/195-003.html
    We have thousands of essays in this area! Below is a list in order of relevance to your search query. All of the following documents are ready for delivery TODAY and priced at only $ /page with a free bibliography! Use the Send Me This Essay link to access our fast, easy order form and receive any essay on this list TODAY!!!... Papers On Meteorology
    Page 4 of 6 Martian Splosh Craters
    send me this essay

    5 pages in length. The universe is full of unique and unusual compositions that help to differentiate one planet from another. Martian splosh craters – also called rampart craters – are one of the most interesting of all, because the way in which they form has had a direct impact upon the shape of Mars as it exists today. Bibliography lists 4 sources.
    Filename: TLCsplsh.rtf
    Ocean Currents and the Overlying Atmospheric Circulation System
    send me this essay

    A 5 page discussion of the relationship between ocean currents and the overlying atmospheric circulation system. Both ocean circulation systems and atmospheric systems have definitive patterns which are comparable in their nature and both function in much the same way in regard to the manner which they move through the world. The author discusses the causes and effects of this interrelationship, noting important phenomena like hurricanes and the ability of the world’s currents to transport not only sedimentary material but man himself. Bibliography lists 3 sources.

    74. Ingenta: Meteorology And Climatology Resources
    Protection Agency ozone depletion glossary http//www.epa.gov/ozone/defns.html. RadarMeteorology Glossary, MIT http//wwwcmpo.mit.edu/Radar_Lab/Glossary.html.
    http://www.ingenta.com/isis/browsing/VisitSubjectResource/ingenta?subject=178

    75. Meteorology, Chemistry And Boundary Layer Studies At Halley
    area for vehicles. meteorology. The three main meteorology programmesrun at Halley are; Recording the weather; Measuring ozone and;
    http://www.antarctica.ac.uk/Living_and_Working/Diaries/Halley/2000/met_images/me
    HOME A-Z index contact BAS comments ... Advanced search
    Meteorology, Chemistry and Boundary Layer Studies at Halley
    Introduction
    Halley has a beautiful position on Earth. It is cold, clean, dry and flat. This makes Halley ideal for many varied and interesting experiments. Of the two science platforms at Halley, one is dedicated to the upper atmosphere and the other to the lower atmosphere, the weather and the ice. These photographs show the team for the winter of 2000, Dan, Alex and Gary and the platform that we work on. Inside the building are computers linked up to the experiments outside, equipment for taking air and water samples, the Dobson Ozone Spectrophotometer (pictured behind us!) and much more. On the roof of our platform is a satellite receiver dish, GPS receivers and a data transmitter. Around the platform are a couple of masts with equipment attached to them, inlet pipes for air samplers and a no-go area for vehicles.
    Meteorology
    The three main meteorology programmes run at Halley are;
    • Recording the weather
    • Measuring ozone and
    • A daily balloon flight
    Recording the weather
    Our weather station at Halley is similar in many respects to any weather station around the world. We have an automatic weather station that measures the temperature, pressure and wind all the time. Every three hours we include our own observations of the weather, cloud cover and visibility. Our observations get sent back to the UK Meteorological Office at Bracknell, and then passed to forecasters who can use our measurements to predict the weather. During the day Dan, Gary and I do the observations and at night whoever is the nightwatchman volunteers to do them for us.

    76. Table Of Continuous Monitoring Sites In The Network
    Community Centre, St. Albans, Carbon Monoxide, Nitrogen Dioxide, PM 10Particulates, ozone, Sulphur Dioxide, meteorology. SB1, South Beds
    http://www.seiph.umds.ac.uk/envhealth/HBNet/hb_table.html
    This table details the continuous monitoring sites which make up the Network. There is also an interactive map of the county showing these sites.
    Site Code Site Name Download Frequency Location Parameters Bedford Background Twice Daily Stewartby, Bedford Ozone, Sulphur Dioxide Broxbourne Roadside Twice Daily Close to M25, Waltham Cross Nitrogen Dioxide, PM Particulates Dacorum Background Hourly Civic Centre, Hemel Hempstead Nitrogen Dioxide, Ozone, PM Particulates, Meteorology East Herts Rural Hourly Throcking, East Herts. Ozone East Herts Background Hourly Sawbridgeworth Nitrogen Dioxide, PM Particulates East Herts Roadside Hourly London Road, Sawbridgeworth Nitrogen Dioxide, PM Particulates Hertsmere Background Twice Daily Furzehill School, Borehamwood Carbon Monoxide, Nitrogen Dioxide, Ozone, PM Particulates, Meteorology Luton Background Hourly Near Junction 11 of the M1 Carbon Monoxide, Nitrogen Dioxide, PM Particulates, Sulphur Dioxide, Meteorology Mid Beds Roadside Hourly High Street, Biggleswade Nitrogen Dioxide (Closed) Mid Beds Rural Hourly Wrest Park, Silsoe

    77. G 304: Physical Meteorology And Climatology Fall 1996
    1. Over the last 30 years ozone has been depleted in a layer of the atmosphere calledthe _ , characterized by temperature
    http://www.indiana.edu/~geog109/exams/109FinExF97.html
    G 109: Weather and Climate Fall 1997 Final Exam PRINT Name: Student Number: You have 2 hours to complete this exam, so pace yourself accordingly. Please be neat!! Total possible points: 100 - 1 point each (check the appropriate box, only one [Total: 16 points]
    • oxygen ozone carbon dioxide hydrogen loss of energy loss of water uptake of latent heat of vaporization release of latent heat of vaporization increase Mie scattering increase Rayleigh scattering increase the solar constant decrease the solar constant an air parcel exerting a force on other air parcels precipitation no energy exchange with its surroundings condensation or evaporation differential heating and expansion the Coriolis effect transfer of latent heat from oceans to land friction at the surface the Earth is closer to the Sun during the Southern Hemisphere summer less area is covered by desert in the Southern Hemisphere a greater proportion of the land surface is mountainous in the Southern Hemisphere there is a greater percentage of water surface in the Southern Hemisphere increase decrease stay constant there is insufficient information to know what will happen climate change release of latent heat the weight of the overlying air energy from the Sun carbon dioxide uptake by green plants solar radiation that is reflected to the surface longwave radiation that is reflected back to the surface by ozone absorption and re-emission of longwave radiation in the atmosphere albedo scattering temperature distance to the sun albedo scattering temperature distance to the sun

    78. Atmosphere
    Atmospheric Chemistry sections on Tropospheric ozone and Stratospheric ozone depletionEnvironmental Effects of ozone Depletion 1998 Weather and meteorology.
    http://www.teachers.ash.org.au/sciencelinks/environment/atmosphere.html
    ScienceLinks: Reviews of quality educational web sites for Science Teachers "Refresh/Reload" for latest additions. Atmosphere and Weather Atmosphere
    Ozone and Ozone Depletion

    Acid Rain

    Weather and Meteorology
    ...
    Teaching Resources

    Atmosphere
    Introduction to Atmospheric Chemistry
    http://www.cac.yorku.ca/intro.html
    York University presents the Introduction to Atmospheric Chemistry Website, a great learning resource for anyone interested in gaining a general idea about atmospheric chemistry. The site is divided into sections including Photochemical Smog/ Tropospheric Ozone, Global Warming, Stratospheric Ozone Depletion, Acidic Deposition, and Toxic Air Pollutants. Each section provides a brief summary and links to related resources. [SN] From the Scout Report for Science and Engineering 17 February, 1999, © Internet Scout Project 1994-1999.
    NCAR: National Center for Atmospheric Research http://www.ncar.ucar.edu/ncar/
    NOAA News http://www.noaanews.noaa.gov/
    [Top]
    Ozone and Ozone Depletion See also: Introduction to Atmospheric Chemistry - sections on Tropospheric ozone and Stratospheric Ozone depletion Environmental Effects of Ozone Depletion: 1998 Assessment [Top] Acid Rain Acid Rain 2000 [Frames, JavaScript]

    79. Atmosphere - Ozone Layer
    by the Cooperative Research Centre (CRC) for Southern Hemisphere meteorology isidentifying key mechanisms that control stratospheric ozone, in particular the
    http://www.environment.vic.gov.au/web/root/domino/gateway/envgate.nsf/viewforms/

    Air Quality
    I Weather I El Nino / La Nina I Ozone Layer Ozone Layer About the Topic
    • Environment Australia - Ozone Protection
      Environment Australia's (EA) Ozone Protection site provides information on ozone and ozone layer depletion including the current status of, and science on, the ozone hole.
      http://www.ea.gov.au/atmosphere/ozone/index.html
    • Ozone Depletion - CSIRO
      The CSIRO Ozone Depletion site provides information on the ozone layer, the ozone "hole" and the effects of ozone depletion.
      http://www.dar.csiro.au/information/ozone.html
    Research
    • CRC for Southern Hemisphere Meteorology
      The Ozone program being undertaken by the Co-operative Research Centre (CRC) for Southern Hemisphere Meteorology is identifying key mechanisms that control stratospheric ozone, in particular the effects of transport, in the southern hemisphere and especially in the Australian region.
      http://www.maths.monash.edu.au/lib/shm_gone.shtml
    What Is Being Done?
    • Methyl Bromide phase-out
      Methyl bromide is a broad-spectrum fumigant, which controls a range of soilborne diseases, insects, nematodes and weeds. It has been classified as a powerful ozone-depleting substance; the bromines it contains are fifty times more destructive to ozone than chlorine (eg. from CFCs). This site contains information about the Australia wide phase out of Methyl Bromide.
    • Ozone Protection in Victoria
      The EPA Victoria site provides information on the Industrial Waste Management Policy (Protection Of The Ozone Layer) which came into operation on 5 November 2001. The policy updates and refines Victoria's management framework for users of ozone-depleting substances to minimise consumption and emissions of these substances.

    80. SpringerLink: Meteorology And Atmospheric Physics - Abstract Volume 75 Issue 3/4
    meteorology and Atmospheric Physics. A vertical profile of ozone concentrationin the atmosphericboundary layer over central Taiwan. WanLi Cheng.
    http://link.springer-ny.com/link/service/journals/00703/bibs/0075003/00750251.ht
    Meteorology and Atmospheric Physics
    ISSN: 0177-7971 (printed version)
    ISSN: 1436-5065 (electronic version) Table of Contents Abstract Volume 75 Issue 3/4 (2000) pp 251-258
    A vertical profile of Ozone concentration in the atmosphericboundary layer over central Taiwan
    Wan-Li Cheng
    Department of Environmental Science, Tunghai University, Taichung 407, Taiwan ROC
    Received April 13, 2000 Revised July 24, 2000 Summary In the central region of Taiwan, ozone episodes occur most often during autumn. Two field experiments were conducted during the autumns of 1998 and 1999 to analyze the vertical profile of the boundary layer and determine its effects on ozone concentration over the region. The vertical virtual potential temperature and wind profiles were derived from tethersonde data. The NO x , NMHC and O concentration vertical profiles were monitored up to a height of 500 meters using black-covered Teflon tedler sampling bags. During the experimental periods, nighttime terrestrial long wave radiation could cause the inversion height to reach 500 meters by the following morning. It was shown that these types of synoptic structures suppress the vertical diffusion of NO x , NMHC and O . During the daytime, measurements indicate that pollutants were well mixed in the upper portion of the mixing layer. At night, the ground level ozone concentration was on the decrease but increased with altitude to a height of 500 m. The NO

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