Urban Air Quality – a Signifi Cant Threat to Human Health?

Total Page:16

File Type:pdf, Size:1020Kb

Urban Air Quality – a Signifi Cant Threat to Human Health? Hannu Talvitie Research Manager Vaisala Helsinki, Finland Urban air quality – A signifi cant threat to human health? Urban air pollution poses a signifi cant the risks that air pollution poses to their diseases. According to the World Bank, threat to human health, the environment citizens. every year an estimated 800,000 people and the quality of life of millions of people On the other hand, such countries die prematurely from lung cancer, in some of the world’s largest cities. (e.g., still face the problem of polluted air even cardiovascular and respiratory diseases New Delhi, Hong Kong, Beijing, Jakarta, though air quality has been improving caused by outdoor air pollution. In Hong Los Angeles and Mexico City). Urbaniza- gradually over the last two decades. For Kong, for example, it is estimated that tion and the associated growth in indus- example, many large cities in Europe still by improving the air quality from the trialization and traffi c have resulted in exceed the specifi c air quality standards existing “average” level to “good” level, the increase of air pollution in densely for ambient pollutants. Th e Helsinki 64,000 hospital days would be saved. populated areas, causing deterioration metropolitan area in Finland, for example, Th ese severe health eff ects are the in air quality. Many cities will need to is one of the cleanest cities in Europe but reason that most countries have already take action to enhance their institutional still the daily limits are exceeded every taken preventative measures to limit and technical capabilities to monitor year. emissions and set limits (called standards) and control air quality and implement for urban air pollutants. City authorities preventive actions in order to reduce How can air pollutants focus on eff orts to reduce emissions and affect human health? monitor levels of air pollutants. A number of epidemiological studies have shown that ambient air pollutants, espe- What are the main cially fi ne and ultra fi ne particulates, pollutants in urban air? have an adverse eff ect on human Scientists have defi ned the main air health. Th is is due to the fact pollutants that pose a health risk for that these tiny particulates humans in urban areas. Th ese pollutants can penetrate deep into are: inhalable particulates (PM10) and the lungs and even be fi ne particulates (PM2.5), nitrogen oxides dissolved in the blood. (NOx), sulphur dioxide (SO₂), ozone (O₃), Th e health eff ects can be carbon monoxide (CO), and lead (Pd). especially hazardous for For each of these pollutants, the World sensitive groups, like Health Organization has defi ned air children, senior citi- quality guidelines for protection against zens, and people with harmful health eff ects. Th e guidelines asthma, obstructive defi ne the specifi c limits or concentra- lung disease (chronic tions that should not be exceeded. Coun- obstructive pulmo- tries often have their own standards that nary disease are similar but the specifi c levels can vary - COPD), and slightly. cardiovascular To measure air quality, networks of monitors record the concentrations of the major pollutants at more than 3,000 locations in the world each day, mostly in developed countries. Th ese raw measure- ments are then converted into Air Quality City authorities focus on e orts to reduce emissions and monitor levels of air pollutants. 4 | Vaisala News 174 / 2 0 07 800 1000 700 900 600 800 700 500 600 400 500 300 400 Altitude (meters) 200 300 200 100 100 0 00 06 12 18 24 Figure 1. Th is picture shows a 1-day measurement of aerosol profi le using the Vaisala Ceilometer CL31 on Nov 22, 2005, in the Helsinki area, Finland. During this day there was a strong inversion that lasted almost the whole day. A high concentration of low level aerosols (particulates from traffi c) can be seen below 100 m, increasing rapidly after 7:30 in the morning. Index (AQI) values. Th e AQI has been to remove it in energy production are that are diff erent from those formed in developed to make it easier for people available and already in common use in burning processes. to understand the signifi cance of moni- most developed countries. (Note: carbon tored and forecast air pollution levels. It dioxide is not counted as a pollutant but How does weather focuses on health eff ects that can take the main greenhouse gas.) affect air quality? place within a few hours or days after Pollution from traffic consists of Changes in day-to-day weather are the breathing polluted air. particulate matter, NOx, CO, volatile greatest factor in controlling the changes An AQI value is calculated for each organic compounds (VOCs), and also in air quality. Weather determines how of the individual pollutants in an area other compounds in small amounts, quickly pollutants are dispersed away (ground-level particulate matter, carbon like polyaromatic hydrocarbons (PAH). from an area and also the thickness of monoxide, sulfur dioxide, nitrogen Lead emission from traffi c has reduced the atmospheric layer (called the mixing dioxide, and ozone). Th e pollutant with dramatically after moving to unleaded height) where the emissions are diluted the highest AQI is used as the overall AQI fuels. Particulates come from the exhaust in a vertical direction. Normally, pollut- reading for that day and is listed as the emissions, especially from diesel engines, ants are mixed with the help of convec- principal pollutant. but also from dust and dirt from roads tion or blown away by wind from their Various agencies around the world and tires. Other fi ne particulates are sources without building up to unsafe measure such indices, though defi ni- formed by chemical reactions in the amounts. But the pollutants can also be tions may vary. Th e index is defi ned so atmosphere. Formation of ozone (O₃) in trapped close to the surface. Th ey cannot that it gives a value of 100 at the specifi c urban areas is mainly caused by traffi c escape, and after a while they may build value of each pollutant. Th e United States pollutants in a photochemical reaction up to unhealthy levels. Th is trapping can Environmental Protection Agency (EPA) with UV radiation from the sun. happen when winds are weak or calm, has determined the AQI scale and health Some of the pollutants also come and when the air close to the ground cools classifi cation as: from natural sources. For example, forest down and warm air moves over, creating fi res emit particulates and VOCs into the a stable condition that keeps pollutants 301 – 500 Hazardous Maroon atmosphere. Volcanoes spew out sulfur close to the surface. Th ese so-called inver- dioxide and large amounts of volcanic sions frequently occur on clear nights. 201 – 300 Very unhealthy Purple ash. Sand storms can also mix particu- Poor air quality can also result from 151 – 200 Unhealthy Red lates into the air from the underlying summer heat. In hot, sunny weather 101 – 150 Unhealthy for sensitive groups Orange ground surface. Vegetation emits VOCs photochemical smog can form 51 – 100 Moderate Yellow 0 – 50 Good Green Particulate Matter (PM) can be divided into four size classes: 1. Large particulates are over 10 microns (>10 µm) in diameter. What are the main 2. PM10 — Particulates under 10 microns (0 – 10 µm) can be inhaled below sources of emission? the nasopharynx area (nose and mouth) and are thus called inhalable Most air pollution comes from human particulates (PM10). activities: burning either fossil fuels (coal, 3. PM2.5 — Particulates that are under 2.5 microns (0 – 2.5 µm) are called oil or natural gas) to power motor vehi- fi ne particulates (PM2.5) and they travel down below the tracheobron- cles and industrial processes, or burning chial region (into the lungs). of biomass to heat houses or produce 4. UFP — Th e smallest particulates are under 0.1 microns (0 – 0.1 µm) and energy. Th e burning processes release are called ultra fi ne particulates (UFP). Th ey can travel in the deepest particulate matter, carbon monoxide, parts of lungs and be dissolved into blood. carbon dioxide (CO₂) and partially burnt hydrocarbon compounds into the atmo- Th e most hazardous size classes to humans are PM2.5 and UFP as they pene- sphere. Depending on the origin of the fuel, trate into the lungs and can even be dissolved into the blood. SO₂ concentrations released in combus- tion vary considerably. Technologies 174 / 2007 Vaisala News | 5 Altitude (Meters) 400 300 200 100 Warmer air Inversion layer Cooler air 0 –20°C 0°C +20°C Temperature through complex chemical reactions tasks is to get more dense and accurate Vaisala radiosondes off er the highest involving NOx, O₃ and VOCs. Photochem- observation data on the mixing height level of temperature, humidity and wind ical smog has a light brown color and can across urban areas to better determine measurement performance for synoptic reduce visibility and aff ect breathing. the air volume where the surface pollut- soundings all over the world. Th ere are Wind can also transport pollution ants are mixed. also special sensor options to measure over long distances. For example, in the Modern air quality models can take ozone and radioactivity profi les in the Helsinki metropolitan area, more than half a variety of data as input: inventory and atmosphere. of the fi ne particulates (PM2.5) are trans- models of emission sources, local disper- Vaisala’s boundary layer profi ler uses ported from outside the country, mainly sion and mixing, weather model and fore- radio frequency (RF) Doppler technique from Central and Eastern Europe.
Recommended publications
  • Meteorological Monitoring Guidance for Regulatory Modeling Applications
    United States Office of Air Quality EPA-454/R-99-005 Environmental Protection Planning and Standards Agency Research Triangle Park, NC 27711 February 2000 Air EPA Meteorological Monitoring Guidance for Regulatory Modeling Applications Air Q of ua ice li ff ty O Clean Air Pla s nn ard in nd g and Sta EPA-454/R-99-005 Meteorological Monitoring Guidance for Regulatory Modeling Applications U.S. ENVIRONMENTAL PROTECTION AGENCY Office of Air and Radiation Office of Air Quality Planning and Standards Research Triangle Park, NC 27711 February 2000 DISCLAIMER This report has been reviewed by the U.S. Environmental Protection Agency (EPA) and has been approved for publication as an EPA document. Any mention of trade names or commercial products does not constitute endorsement or recommendation for use. ii PREFACE This document updates the June 1987 EPA document, "On-Site Meteorological Program Guidance for Regulatory Modeling Applications", EPA-450/4-87-013. The most significant change is the replacement of Section 9 with more comprehensive guidance on remote sensing and conventional radiosonde technologies for use in upper-air meteorological monitoring; previously this section provided guidance on the use of sodar technology. The other significant change is the addition to Section 8 (Quality Assurance) of material covering data validation for upper-air meteorological measurements. These changes incorporate guidance developed during the workshop on upper-air meteorological monitoring in July 1998. Editorial changes include the deletion of the “on-site” qualifier from the title and its selective replacement in the text with “site specific”; this provides consistency with recent changes in Appendix W to 40 CFR Part 51.
    [Show full text]
  • The Tropical Rainfall Measuring Mission (TRMM) Progress Report
    The Tropical Rainfall Measuring Mission (TRMM) Progress Report Joanne Simpson Christian D. Kummerow Robert Meneghini Arthur Hou Robert F. Adler NASA Goddard Space Flight Center George Huffman Science Systems & Applications Inc. Bruce Barkstrom Bruce Wielicki NASA Langley Research Center Steven J. Goodman Hugh Christian NASA Marshall Space Flight Center Toshi Kozu Shimane University Shimane, Japan T. N. Krishnamurti Song Yang Florida State University Brad Ferrier Joint Center for Environmental Technology, University of Maryland at Baltimore ii Abstract Recognizing the importance of rain in the tropics and the accompanying latent heat release, NASA for the U.S. and NASDA for Japan have partnered in the design, construction and flight of an Earth Probe satellite to measure tropical rainfall and calculate the associated heal_g. Primary mission goals are 1) the understanding of crucial links in climate variability by the hydrological cycle, 2) improvement in the large-scale models of weather and climate 3) Improvement in understanding cloud ensembles and their impacts on larger scale circulations. The linkage with the tropical oceans and landmasses are also emphasized. The Tropical Rainfall Measuring Mission (TRMM) satellite was launched in November 1997 with fuel enough to Obtain a four to five year data set of rainfall over the global tropics from 37°N to 37°S. This paper reports progress from launch date through the spring of 1999. The data system and its products and their access is described, as are the algorithms used to obtain the data. Some exciting early results from TRMM are described. Some important algorithm improvements are shown. These will be used in the first total data reprocessing, scheduled to be complete in early 2000.
    [Show full text]
  • Data Requirements for Ceiling and Visibility Products Development 6
    DOT/FAA/RD-94/5 Project Report ATC-212 Data Requirements for Ceiling and Visibility Products Development J. L. Keller 13 April 1994 Lincoln Laboratory MASSACHUSETTS INSTITUTE OF TECHNOLOGY LEXINGTON, MASSACHUSETTS Prepared for the Federal Aviation Administration, Washington, D.C. 20591 This document is available to the public through the National Technical Information Service, Springfield, VA 22161 This document is disseminated under the sponsorship of the Department of Transportation in the interest of information exchange. The United States Government assumes no liability for its contents or use thereof. TECHNICAL REPORT STANDARD TITLE PAGE 1. Report No. 2. Government Accession No. 3. Recipient's Catalog No. ATC-212 DOTfFAAJRD-94/5 4. TItle and Subtitle 5. Report Date 13 April 1994 Data Requirements for Ceiling and Visibility Products Development 6. Performing Organization Code 7. Author(s) 8. Performing Organization Report No. John L. Keller ATC-212 9. Performing Organization Name and Address 10. Work Unit No. (TRAIS) Lincoln Lahoratory, MIT P.O. Box 73 11. Contract or Grant No. Lexington, MA 02173-9108 DTFAO1-93-Z-02012 12. Sponsoring Agency Name and Address 13. Type of Report and Period Covered Department of Transportation Project Report Federal Aviation Administration Washington, DC 20591 14. Sponsoring Agency Code 15. Supplementary Notes This report is hased on studies performed at Lincoln Laboratory, a center for research operated hy Massachusetts Institute of Technology. The work was sponsored hy the Air Force under Contract Fl9628-90-C-0002. 16. Abstract The Federal Aviation Administration (FAA) Integrated Terminal Weather System (ITWS) is supporting the development of weather products important for air traffic control in the terminal area.
    [Show full text]
  • Evaluation of ARM Tethered Balloon System Instrumentation For
    Atmos. Meas. Tech. Discuss., https://doi.org/10.5194/amt-2019-117 Manuscript under review for journal Atmos. Meas. Tech. Discussion started: 7 May 2019 c Author(s) 2019. CC BY 4.0 License. Evaluation of ARM Tethered Balloon System instrumentation for supercooled liquid water and distributed temperature sensing in mixed-phase Arctic clouds Darielle Dexheimer1, Martin Airey2, Erika Roesler1, Casey Longbottom1, Keri Nicoll2,5, Stefan Kneifel3, Fan Mei4, R. Giles Harrison2, Graeme Marlton2, Paul D. Williams2 5 1Sandia National Laboratories, Albuquerque, New Mexico, USA 2University of Reading, Dept. of Meteorology, Reading, UK 3University of Cologne, Institute for Geophysics and Meteorology, Cologne, Germany 4Pacific Northwest National Laboratory, Richland, Washington, USA 5University of Bath, Dept. of Electronic and Electrical Engineering, Bath, UK 10 Correspondence to: Darielle Dexheimer ([email protected]) Abstract. A tethered balloon system (TBS) has been developed and is being operated by Sandia National Laboratories (SNL) on behalf of the U.S. Department of Energy’s (DOE) Atmospheric Radiation Measurement (ARM) User Facility in order to collect in situ atmospheric measurements within mixed-phase Arctic clouds. Periodic tethered balloon flights have been 15 conducted since 2015 within restricted airspace at ARM’s Advanced Mobile Facility 3 (AMF3) in Oliktok Point, Alaska, as part of the AALCO (Aerial Assessment of Liquid in Clouds at Oliktok), ERASMUS (Evaluation of Routine Atmospheric Sounding Measurements using Unmanned Systems), and POPEYE (Profiling at Oliktok Point to Enhance YOPP Experiments) field campaigns. The tethered balloon system uses helium-filled 34 m3 helikites and 79 and 104 m3 aerostats to suspend instrumentation that is used to measure aerosol particle size distributions, temperature, horizontal wind, pressure, relative 20 humidity, turbulence, and cloud particle properties and to calibrate ground-based remote sensing instruments.
    [Show full text]
  • Article in Press
    ARTICLE IN PRESS Atmospheric Environment xxx (2009) 1–10 Contents lists available at ScienceDirect Atmospheric Environment journal homepage: www.elsevier.com/locate/atmosenv Nocturnal boundary layer characteristics and land breeze development in Houston, Texas during TexAQS II Bridget M. Day a, Bernhard Rappenglu¨ ck a,*, Craig B. Clements a,1, Sara C. Tucker b,c, W. Alan Brewer c a Department of Earth and Atmospheric Sciences, University of Houston, 4800 Calhoun Rd, Houston, TX 77204-5007, USA b Cooperative Institute for Research in Environmental Sciences, University of Colorado at Boulder, 325 Broadway, Boulder, CO 80305, USA c NOAA Earth System Research Laboratory, 325 Broadway, Boulder, CO 80305, USA article info abstract Article history: The nocturnal boundary layer in Houston, Texas was studied using a high temporal and vertical reso- Received 4 September 2008 lution tethersonde system on four nights during the Texas Air Quality Study II (TexAQS II) in August and Received in revised form September 2006. The launch site was on the University of Houston campus located approximately 4 km 14 January 2009 from downtown Houston. Of particular interest was the evolution of the nocturnal surface inversion and Accepted 25 January 2009 the wind flows within the boundary layer. The land–sea breeze oscillation in Houston has important implications for air quality as the cycle can impact ozone concentrations through pollutant advection and Keywords: recirculation. The results showed that a weakly stable surface inversion averaging in depth between 145 TexAQS II Tethersonde and 200 m AGL formed on each of the experiment nights, typically within 2–3 h after sunset.
    [Show full text]
  • Speaker Abstracts
    Appendix E: Speaker Abstracts 100 Years of Progress in Boundary-Layer Meteorology: A look to the past, questions for the future Margaret A. LeMone NCAR (with contributions from Wayne Angevine, Fei Chen, Jimy Dudhia, Kristina Katsaros, Larry Mahrt, Jielun Sun, and Michael Tjernstrom)1 and input from Chris Fairall, Jim Fleming, Ned Patton, Shuyi Chen, and Peter Sullivan2 We define the atmospheric boundary-layer (ABL) as that layer of air directly influenced by exchange of heat and energy with the surface. Our story of the ABL begins with surface fluxes, which are dependent on surface roughness and the exchange of energy between the surface and atmosphere. The ABL is typically divided into a surface layer, through which shear production of turbulence kinetic energy is as important as buoyancy production, a well-mixed inner layer, and a transition layer that is alternately occupied by turbulent and free-atmosphere air. This division is most straightforward for a cloudless, steady-state, unstable ABL. Our history begins with the classical-physics roots from the 18th and 19th Centuries and their early applications to the atmospheric boundary layer, and the contributions from the early turbulence/boundary layer community, who developed the concept of the boundary layer and applied it to flow through wind tunnels, past aircraft wings, and sometimes in the atmosphere itself, with some reference to early discoveries from those more interested in agricultural applications. From there, we examine the boundary layer from the surface on up, through a look at our understanding of the surface energy budget, exchange coefficients and flux-profile relationships in the surface layer over land and ocean, and the study of the entire cloud-free ABL under unstable and stable conditions.
    [Show full text]
  • South Central Coast Cooperative Aerometric Monitoring Program
    Walter F. Dabberdt1 and South Central Coast Cooperative William Viezee2 Aerometric Monitoring Program (SCCCAMP) Abstract The SCCCAMP field measurement program, conducted 3 September to 7 October 1985, is the most comprehensive mesoscale photochemical study of its type ever undertaken. The study area encompasses 2 X 104 km2 of coastal and interior south-central California including the Santa Barbara Channel. A review of earlier experimental and analytical studies in the area is followed by the organizational framework and planning for this cooperative program. The experimental design and measurement systems are described. Existing ground-based meteoro- logical and air pollution networks were supplemented by additional surface aerometric stations, dual Doppler radars, rawinsondes, and a network of Doppler acoustic profilers. Airborne measurement platforms included one dual-channel lidar, three aerometric sampling aircraft,3 and a meteorological research aircraft. Gas tracer tests included 4-h releases of three perfluorocarbon gas tracers. Tracer measurements were FIG. 1. Topographic map of SCCCAMP region. made over two-day periods at 50 surface locations and aloft by aircraft with a near-realtime two-trap chromatographic system. Four multi-day The SCCCAMP area has been the focus of intensive at- intensive operational periods (IOP) are described, and illustrative re- mospheric research studies for more than two decades during sults from one IOP are presented when extremely high ozone concen- trations were observed at ground level (230 ppb) and aloft (290 ppb). which numerous meteorological, air pollution, and gas-tracer The availability of the composite data base is indicated. measurement and analysis programs have been conducted. Edinger (1963) used aircraft soundings to investigate the mod- ification of the marine boundary layer (MBL) as it is advected through the Santa Clara River Valley.
    [Show full text]
  • CIMMS Annual Report FY08
    Cooperative Institute for Mesoscale Meteorological Studies Annual Report Prepared for the National Oceanic and Atmospheric Administration Office of Oceanic and Atmospheric Research Cooperative Agreement NA16OAR4320115 Fiscal Year – 2017 1 Cover image – Images from the Hazard Services – Probabilistic Hazard Information (HS-PHI) 2017 spring experiment in the NOAA Hazardous Weather Testbed, including various forecaster and researcher interactions with the software and during group discussions. Also shown is a screen capture of the HS-PHI application, showing probabilistic tornado “plumes” for a Quasi- Linear Convective System (QLCS). For more on this project, “Hazard Services – Probabilistic Hazard Information (HS-PHI)”, involving Greg Stumpf (CIMMS at OST/MDL/DAB) and Tiffany Meyers (CIMMS at NSSL), see pages 143-145. 2 Table of Contents Introduction 4 General Description of CIMMS and its Core Activities 4 Management of CIMMS, including Mission and Vision Statements, and Organizational Structure 5 Executive Summary Listing of Activities during FY2017 6 Distribution of NOAA Funding by CIMMS Task and Research Theme 11 CIMMS Executive Board and Assembly of Fellows Meeting Dates and Membership 12 General Description of Task I Expenditures 14 Research Performance 15 Theme 1 – Weather Radar Research and Development 15 Theme 2 – Stormscale and Mesoscale Modeling Research and Development 55 Theme 3 – Forecast and Warning Improvements Research and Development 104 Theme 4 – Impacts of Climate Change Related to Extreme Weather Events 176 Theme 5 –
    [Show full text]
  • UNSTABLE the Understanding Severe Thunderstorms and Alberta Boundary Layers Experiment ______Scientific Overview
    UNSTABLE The UNderstanding Severe Thunderstorms and Alberta Boundary Layers Experiment _______________________________________ Scientific Overview Neil Taylor1, David Sills2, John Hanesiak3, Jason Milbrandt4, Craig Smith5, Pat McCarthy6, Geoff Strong7 1Hydrometeorology and Arctic Lab, Environment Canada 2Cloud Physics and Severe Weather Research Section and Nowcasting and Remote Sensing Lab, Environment Canada 3Centre for Earth Observation Science (CEOS), University of Manitoba 4Recherche en Prévision Numérique [RPN] (Numerical Weather Prediction Research Section), Environment Canada 5Climate Research Division, Environment Canada 6Prairie and Arctic Storm Prediction Centre, Environment Canada 7University of Alberta (Adjunct) 2 Table of Contents List of Figures ................................................................................................................................. 4 List of Tables .................................................................................................................................. 6 List of Abbreviations .................................................................................................................... 7 2. Rationale for UNSTABLE ........................................................................................................ 9 2.1 Socio-economic Impacts of Severe Weather in Alberta ..................................................... 9 2.2 Summer Severe Weather Forecast Challenges ............................................................... 11 2.3 Relationship
    [Show full text]
  • 2Nd Quarter Publications
    NOAA Air Resources Laboratory Quarterly Activity Report FY2017 Quarter 2 (January-February-March, 2017) Contents: Dispersion and Boundary Layer 1. HYSPLIT 2. Unmanned Aircraft Systems and VORTEX-SE 3. Project Sagebrush 4. Wind Forecast Improvement Project (WFIP2) 5. HYSPLIT for Annual DOE Assessments 6. Consequence Assessment for the Nevada National Security Site 7. SORD Mesonet 8. Support to DOE/NNSA NNSS Projects and Experiments Atmospheric Chemistry and Deposition 9. Fluxes of Greenhouse Gases in Maryland (FLAGG-MD) project 10. Atmospheric Mercury Modeling Climate Observations and Analyses 11. Climate Reference Network (CRN) 12. NOAA/INL Mesonet ARL 2nd Quarter Publications Conference Presentations & Invited Talks Outreach & Engagement DISPERSION AND BOUNDARY LAYER 1. HYSPLIT In 2016, over one million (1,094,305) HYSPLIT simulations were performed on the READY web server (http://www.ready.noaa.gov), exceeding the previous record set in 2014 (1,020,081). HYSPLIT simulations have seen a steady increase since 2009 when statistics were started for user’s HYSPLIT runs. READY users can create air parcel trajectories or air concentration maps with HYSPLIT using archived or forecast meteorological data, although the primary HYSPLIT simulation has been trajectories using archived meteorological data. READY is celebrating is 20th year. An ARL Highlight has been posted (www.arl.noaa.gov). [email protected] The HYSPLIT computer code was delivered to NCEP for operational implementation coincident with NCEP's Global Forecast System (GFS) model upgrade planned for June 2017. This was a relatively minor HYSPLIT upgrade since only changes related to the global meteorological models were implemented. ARL scientists closely collaborated with NCEP to generate HYSPLIT-formatted files from the GFS model output on the GFS native vertical levels, in contrast to the more coarse, but traditional, meteorological pressure levels.
    [Show full text]
  • 070410 COPS Instrumentation
    COPS Instrumentation Version 10 April 2007 Table of Contents 1 Airborne Platforms and Instruments .......................................................................................................................... 3 1.1 DLR Falcon with Water-Vapour DIAL, Wind Lidar, and Dropsondes ............................................................ 3 1.2 SAFIRE Falcon ................................................................................................................................................. 6 1.3 Research Aircraft DO 128 (IBUF) .................................................................................................................... 6 1.4 BAe146 ........................................................................................................................................................... 10 1.5 Learjet 35A...................................................................................................................................................... 10 1.6 Zeppelin NT with AirLIF ................................................................................................................................ 10 1.7 UltraLight ........................................................................................................................................................ 13 1.8 Dimona ............................................................................................................................................................ 13 1.9 Parternavia......................................................................................................................................................
    [Show full text]
  • Downloaded 10/11/21 06:11 AM UTC Lidars During Nighttime Intensive Observational Peri- Ods (Iops)
    THE METCRAX II FIELD EXPERIMENT A Study of Downslope Windstorm-Type Flows in Arizona’s Meteor Crater BY MANUELA LEHNER, C. DAVID WHITEMAN, SEBASTIAN W. HOCH, ERIK T. CROsmAN, MATTHEW E. JEGLUM, NIHANTH W. CHERUKURU, RONALD CALHOUN, BIANCA ADLER, NORBERT KALTHOFF, RICHARD ROTUNNO, THOMAS W. HORST, STEVEN SEmmER, WILLIAM O. J. BROWN, STEVEN P. ONCLEY, ROLAND VOGT, A. MARTINA GRUDZIELANEK, JAN CERMAK, NILS J. FONTEYNE, CHRISTIAN BERNHOFER, ANDREA PITAccO, AND PETRA KLEIN The METCRAX II field investigation of downslope windstorm–type flows in Arizona’s Meteor Crater is described along with first results from the analyses of the extensive dataset. he second Meteor Crater Experiment (METCRAX 2008). On several nights during METCRAX I, high II) meteorological field campaign was conducted wind speeds and strong turbulence were encountered T in October 2013 in and around the Barringer over the west sidewall, while the east sidewall and the Meteorite Crater (also known as Meteor Crater) crater center seemed to remain unaffected. At the near Winslow, Arizona (Fig. 1). The experiment was same time, observed temperatures over the west side- designed to investigate a phenomenon that was dis- wall were much higher than over the rest of the crater covered serendipitously during the first METCRAX basin. Subsequent analysis revealed that these events experiment of 2006, which was focused on an inves- are produced by the interaction of a southwesterly, tigation of the stable nighttime boundary layer that mesoscale katabatic flow, which forms on the plain
    [Show full text]