PM2.5 Pollution and Temperature Inversions: a Case Study in St
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The Art and Science of Forecasting Morning Temperature Inversions by Anthony J
Air Quality Forecasting Excl usive Con tent The Art and Science of Forecasting Morning Temperature Inversions by Anthony J. Sadar Anthony J. Sadar is a Certified Consulting Meteorologist and Air Pollution Administrator with the Allegheny County Health Department, Air Quality Program in Pittsburgh, PA. E-mail: [email protected]. The author provides an overview of the key resources and variables used to produce morning surface air inversion forecasts in Pittsburgh, PA. Although the focus is southwestern Pennsylvania, the forecasting approach can be applied to similar locations across the globe. Air quality in southwestern Pennsylvania, as in most other areas of the Accurate forecasting of the onset of an inversion would benefit areas world, is very much influenced by surface-based temperature inver - prone to strong and/or persistent inversions. Advanced notice of im - sions. An atmospheric temperature inversion occurs when air temper - pending stagnant air conditions would give government regulators, ature increases with increasing height. In the layer of air nearest the industry operators, and the public time to mitigate emissions, and earth’s surface—the troposphere—this situation is the inverse of the hence, pollutant concentrations, as well as reduce exposure to “normal” condition where a warm ground keeps low-lying air warmer elevated pollution levels. than air higher up. Normally then, the warm surface air can rise and the cool air aloft can descend, causing the atmosphere to mix. Detecting Inversions To collect temperature, wind, and other data with height, the National A surface-based (or ground-level) temperature inversion forms Weather Service (NWS) releases a balloon-borne measurement trans - when air close to the ground cools faster than air at a higher altitude. -
Global Disease and Air Quality in a Changing Climate by Kim Frauhammer
YP Perspective Global Disease and Air Quality in a Changing Climate by Kim Frauhammer Through the lens of the current global pandemic, a look at some of the existing challenges, such as environmental degradation, decreasing air quality, and climate change, that continue to put the human population at risk. 2020 has already been a year to remember, defined by the Seasonality of the Virus novel Coronavirus and its far-reaching effects on our health With how expansive this virus has proven to be, examining and economy. This global pandemic has restructured our all methods of transport is vital to understanding the future lives, while existing global challenges that continue to put the of global diseases. According to the U.S. Global Change human population at risk remain. Environmental degradation, Research Program, a set of “vulnerability factors” determine decreasing air quality, and climate change continue to expose whether someone is at risk for adverse health outcomes: the human population to higher risks of illness and loss of exposure, sensitivity, and adaptive capacity.1 The climate and resources. COVID-19 has provided us with a unique window environment are a part of all three. The virus first emerged into identifying these underlying risks and highlights the and spread rampantly during the Northern Hemisphere benefits between preserving the future of not only our Winter and there is scientific evidence to point to why. health, but our environment as well. Humidity is the greatest factor. em • The Magazine for Environmental Managers • A&WMA • August 2020 YP Perspective In the midlatitudes of the Northern Hemisphere (broadly be - Recent research from Harvard University cites that people tween 30 and 60 degrees), the atmosphere cools down as the who live in areas of poor air quality are more likely to die Earth is tilted farther away from the sun during the winter. -
An Air Stagnation Index to Qualify Extreme Haze Events in Northern China
OCTOBER 2018 F E N G E T A L . 3489 An Air Stagnation Index to Qualify Extreme Haze Events in Northern China JIN FENG Institute of Urban Meteorology, China Meteorological Administration, Beijing, China, and National Center for Atmospheric Research, Boulder, Colorado JIANNONG QUAN Institute of Urban Meteorology, China Meteorological Administration, Beijing, China HONG LIAO Jiangsu Key Laboratory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, School of Environmental Science and Engineering, Nanjing University of Information Science and Technology, Nanjing, China YANJIE LI State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China XIUJUAN ZHAO Institute of Urban Meteorology, China Meteorological Administration, Beijing, China (Manuscript received 27 November 2017, in final form 18 June 2018) ABSTRACT Stagnation weather affects atmospheric diffusion ability, and hence causes the occurrence of haze events, which have been happening frequently in northern China (NC). This work puts forward an air stagnation index (ASITS) to characterize the stagnation weather in NC, in which the processes of ventilation, vertical diffusion, and wet deposition potency are concerned. ASITS can be applied to analyze air stagnation conditions with daily to monthly time scale. It is shown that the ASITS and particulate matter smaller than 2.5 mmindiameter(PM2.5) concen- trations own similar lognormal probability distribution functions on both daily and monthly time scales. And the correlation analyses between the ASITS and PM2.5 concentrations indicate that the ASITS can reflect the monthly and daily variations in PM2.5 concentrations in NC. -
ESSENTIALS of METEOROLOGY (7Th Ed.) GLOSSARY
ESSENTIALS OF METEOROLOGY (7th ed.) GLOSSARY Chapter 1 Aerosols Tiny suspended solid particles (dust, smoke, etc.) or liquid droplets that enter the atmosphere from either natural or human (anthropogenic) sources, such as the burning of fossil fuels. Sulfur-containing fossil fuels, such as coal, produce sulfate aerosols. Air density The ratio of the mass of a substance to the volume occupied by it. Air density is usually expressed as g/cm3 or kg/m3. Also See Density. Air pressure The pressure exerted by the mass of air above a given point, usually expressed in millibars (mb), inches of (atmospheric mercury (Hg) or in hectopascals (hPa). pressure) Atmosphere The envelope of gases that surround a planet and are held to it by the planet's gravitational attraction. The earth's atmosphere is mainly nitrogen and oxygen. Carbon dioxide (CO2) A colorless, odorless gas whose concentration is about 0.039 percent (390 ppm) in a volume of air near sea level. It is a selective absorber of infrared radiation and, consequently, it is important in the earth's atmospheric greenhouse effect. Solid CO2 is called dry ice. Climate The accumulation of daily and seasonal weather events over a long period of time. Front The transition zone between two distinct air masses. Hurricane A tropical cyclone having winds in excess of 64 knots (74 mi/hr). Ionosphere An electrified region of the upper atmosphere where fairly large concentrations of ions and free electrons exist. Lapse rate The rate at which an atmospheric variable (usually temperature) decreases with height. (See Environmental lapse rate.) Mesosphere The atmospheric layer between the stratosphere and the thermosphere. -
Anticyclones
Anticyclones Background Information for Teachers “High and Dry” A high pressure system, also known as an anticyclone, occurs when the weather is dominated by stable conditions. Under an anticyclone air is descending, maybe linked to the large scale pattern of ascent and descent associated with the Global Atmospheric Circulation, or because of a more localized pattern of ascent and descent. As shown in the diagram below, when air is sinking, more air is drawn in at the top of the troposphere to take its place and the sinking air diverges at the surface. The diverging air is slowed down by friction, but the air converging at the top isn’t – so the total amount of air in the area increases and the pressure rises. More for Teachers – Anticyclones Sinking air gets warmer as it sinks, the rate of evaporation increases and cloud formation is inhibited, so the weather is usually clear with only small amounts of cloud cover. In winter the clear, settled conditions and light winds associated with anticyclones can lead to frost. The clear skies allow heat to be lost from the surface of the Earth by radiation, allowing temperatures to fall steadily overnight, leading to air or ground frosts. In 2013, persistent High pressure led to cold temperatures which caused particular problems for hill sheep farmers, with sheep lambing into snow. In summer the clear settled conditions associated with anticyclones can bring long sunny days and warm temperatures. The weather is normally dry, although occasionally, localized patches of very hot ground temperatures can trigger thunderstorms. An anticyclone situated over the UK or near continent usually brings warm, fine weather. -
Synoptic Meteorology
Lecture Notes on Synoptic Meteorology For Integrated Meteorological Training Course By Dr. Prakash Khare Scientist E India Meteorological Department Meteorological Training Institute Pashan,Pune-8 186 IMTC SYLLABUS OF SYNOPTIC METEOROLOGY (FOR DIRECT RECRUITED S.A’S OF IMD) Theory (25 Periods) ❖ Scales of weather systems; Network of Observatories; Surface, upper air; special observations (satellite, radar, aircraft etc.); analysis of fields of meteorological elements on synoptic charts; Vertical time / cross sections and their analysis. ❖ Wind and pressure analysis: Isobars on level surface and contours on constant pressure surface. Isotherms, thickness field; examples of geostrophic, gradient and thermal winds: slope of pressure system, streamline and Isotachs analysis. ❖ Western disturbance and its structure and associated weather, Waves in mid-latitude westerlies. ❖ Thunderstorm and severe local storm, synoptic conditions favourable for thunderstorm, concepts of triggering mechanism, conditional instability; Norwesters, dust storm, hail storm. Squall, tornado, microburst/cloudburst, landslide. ❖ Indian summer monsoon; S.W. Monsoon onset: semi permanent systems, Active and break monsoon, Monsoon depressions: MTC; Offshore troughs/vortices. Influence of extra tropical troughs and typhoons in northwest Pacific; withdrawal of S.W. Monsoon, Northeast monsoon, ❖ Tropical Cyclone: Life cycle, vertical and horizontal structure of TC, Its movement and intensification. Weather associated with TC. Easterly wave and its structure and associated weather. ❖ Jet Streams – WMO definition of Jet stream, different jet streams around the globe, Jet streams and weather ❖ Meso-scale meteorology, sea and land breezes, mountain/valley winds, mountain wave. ❖ Short range weather forecasting (Elementary ideas only); persistence, climatology and steering methods, movement and development of synoptic scale systems; Analogue techniques- prediction of individual weather elements, visibility, surface and upper level winds, convective phenomena. -
Thermal Inversion and Particulate Matter Concentration in Wrocław in Winter Season
atmosphere Article Thermal Inversion and Particulate Matter Concentration in Wrocław in Winter Season Jadwiga Nidzgorska-Lencewicz * and Małgorzata Czarnecka Department of Environmental Management, West Pomeranian University of Technology in Szczecin, ul. Papie˙zaPawła VI, 71-459 Szczecin, Poland; [email protected] * Correspondence: [email protected] Received: 15 October 2020; Accepted: 7 December 2020; Published: 12 December 2020 Abstract: Studies on air quality frequently adopt clustering, in particular the k-means technique, owing to its simplicity, ease of implementation and efficiency. The aim of the present paper was the assessment of air quality in a winter season (December–February) in the conditions of temperature inversion using the k-means method, representing a non-hierarchical algorithm of cluster analysis. The air quality was assessed on the basis of the concentrations of particulate matter (PM10, PM2.5). The studies were conducted in four winter seasons (2015/16, 2016/17, 2017/18, 2019/20) in Wrocław (Poland). As a result of the application of the v-fold cross test, six clusters for each fraction of PM were identified. Even though the analysis covers only four winter seasons, the applied method has unequivocally revealed that the characteristics of surface-based (SBI) and elevated inversions (ELI) affect the concentration level of both fractions of particulate matter. In the case of PM10, the average lowest daily concentration (15.5 µg m 3) was recorded in the conditions of approx. 205 m in thickness, · − 0.5 ◦C intensity of the SBI and at the height of the base of the ELI at approx. 1700 m a.g.l., a thickness of 148 m and an intensity of 1.2 C. -
Temperature Inversions.Pdf
MID-ATLANTIC dronesKnowledge Elevated TEMPERATURE WHAT DOES IT MEAN FOR THE UAV PILOT? HOW DOES IT AFFECT THE WEATHER? INVERSION midatlanticdrones.com #TEMPERATUREINVERSION Temperature inversion: a layer of cool air at the surface is overlain by a layer of warmer air NORMAL CONDITIONS TEMPERATURE INVERSION COLD AIR COLD AIR COLD AIR COLD AIR WARMER AIR WARMER AIR COOLER AIR COOLER AIR WARMER AIR WARMER AIR COOLER AIR COOLER AIR On the left, arrows show normal conditions: Warm air rises and normal convective patterns persist. During temperature inversion, shown on the right, the warm air acts like a cap, shutting down convection and trapping smog over the city. #TEMPERATUREINVERSION warm air on top of cold air Expect fog and haze temp/dew point spread is low little convection – A temperature inversion means some warm air on top of some cold air. – The cold air underneath on the ground, along with a high relative humidity, means you are expecting fog in the cooler area. – If you check the METARS for the airports in the area as you will most likely have a temperature/dewpoint spread that is low. – The air will be smooth because there is little convection. #TEMPERATUREINVERSION 3 what does this mean for you, the drone pilot? Temperature inversions can represent an important element of air pollution, especially in places that are inhabitted, and in valleys. The warmer air layer acts as a natural lid that keeps pollution and dirt trapped. This trapped layer of dirty air stays in there unable to escape. The main issue for UAVs is visibility. -
Glossary of Severe Weather Terms
Glossary of Severe Weather Terms -A- Anvil The flat, spreading top of a cloud, often shaped like an anvil. Thunderstorm anvils may spread hundreds of miles downwind from the thunderstorm itself, and sometimes may spread upwind. Anvil Dome A large overshooting top or penetrating top. -B- Back-building Thunderstorm A thunderstorm in which new development takes place on the upwind side (usually the west or southwest side), such that the storm seems to remain stationary or propagate in a backward direction. Back-sheared Anvil [Slang], a thunderstorm anvil which spreads upwind, against the flow aloft. A back-sheared anvil often implies a very strong updraft and a high severe weather potential. Beaver ('s) Tail [Slang], a particular type of inflow band with a relatively broad, flat appearance suggestive of a beaver's tail. It is attached to a supercell's general updraft and is oriented roughly parallel to the pseudo-warm front, i.e., usually east to west or southeast to northwest. As with any inflow band, cloud elements move toward the updraft, i.e., toward the west or northwest. Its size and shape change as the strength of the inflow changes. Spotters should note the distinction between a beaver tail and a tail cloud. A "true" tail cloud typically is attached to the wall cloud and has a cloud base at about the same level as the wall cloud itself. A beaver tail, on the other hand, is not attached to the wall cloud and has a cloud base at about the same height as the updraft base (which by definition is higher than the wall cloud). -
Asthma Aggravation, Combustion, and Stagnant Air
466 Thorax 2000;55:466–470 Asthma aggravation, combustion, and stagnant air Gary Norris, Timothy Larson, Jane Koenig, Candis Claiborn, Lianne Sheppard, Dennis Finn Abstract meteorology with a knowledge of specific air Background—The relationship between pollution point sources. current concentrations of ambient air Other studies have combined meteorology pollution and adverse health eVects is with chemical composition of particulate mat- controversial. We report a meteorological ter. For instance, factor analysis with a varimax index of air stagnation that is associated rotation of the particulate matter composition with daily visits to the emergency depart- collected from 1957 to 1961 from 30 cities ment for asthma in two urban areas. across the USA found seven factors represent- Methods—Data on daily values of a stag- ing heavy industry or steel production, internal nation persistence index and visits to the combustion engines, coal combustion, possible emergency department for asthma were gas production, a zinc-tin factor, plating, and collected for approximately two years in copper.6 Gatz7 included meteorological vari- Spokane, Washington, USA and for 15 ables (mean wind speed, maximum wind months in Seattle, Washington, USA. The speed, ventilation rate, wind direction, rain) stagnation persistence index represents along with the composition of particulate mat- the number of hours during the 24 hour ter in a factor analysis to help identify sources. day when surface wind speeds are less In that study wind direction was the only than the annual hourly median value, an meteorological variable that was correlated index readily available for most urban with particulate matter concentration. 8 areas. Associations between the daily Thurston and Spengler used factor analysis stagnation persistence index and daily with a varimax rotation separately on particu- emergency department visits for asthma late matter composition and meteorological were tested using a generalised additive parameters. -
Key Points in Air Pollution Meteorology
International Journal of Environmental Research and Public Health Review Key Points in Air Pollution Meteorology Isidro A. Pérez * , Mª Ángeles García , Mª Luisa Sánchez, Nuria Pardo and Beatriz Fernández-Duque Department of Applied Physics, Faculty of Sciences, University of Valladolid, Paseo de Belén, 7, 47011 Valladolid, Spain; [email protected] (M.Á.G.); [email protected] (M.L.S.); [email protected] (N.P.); [email protected] (B.F.-D.) * Correspondence: [email protected] Received: 22 September 2020; Accepted: 9 November 2020; Published: 11 November 2020 Abstract: Although emissions have a direct impact on air pollution, meteorological processes may influence inmission concentration, with the only way to control air pollution being through the rates emitted. This paper presents the close relationship between air pollution and meteorology following the scales of atmospheric motion. In macroscale, this review focuses on the synoptic pattern, since certain weather types are related to pollution episodes, with the determination of these weather types being the key point of these studies. The contrasting contribution of cold fronts is also presented, whilst mathematical models are seen to increase the analysis possibilities of pollution transport. In mesoscale, land–sea and mountain–valley breezes may reinforce certain pollution episodes, and recirculation processes are sometimes favoured by orographic features. The urban heat island is also considered, since the formation of mesovortices determines the entry of pollutants into the city. At the microscale, the influence of the boundary layer height and its evolution are evaluated; in particular, the contribution of the low-level jet to pollutant transport and dispersion. -
10-519 WFO Air Quality Products Specification
Department of Commerce • National Oceanic & Atmospheric Administration • National Weather Service NATIONAL WEATHER SERVICE INSTRUCTION 10-519 October 10, 2017 Operations and Services Public Weather Services, NWSPD 10-5 WFO AIR QUALITY PRODUCTS SPECIFICATION NOTICE: This publication is available at: http://www.nws.noaa.gov/directives/. OPR: W/AFS21 (J. Ferrell) Certified by: W/AFS21 (M. Hawkins) Type of Issuance: Routine SUMMARY OF REVISIONS: This directive supersedes NWSI 10-519, “WFO Air Quality Products Specification,” dated August 31, 2013. Changes made to reflect NWS Headquarters reorganization effective April 1, 2015. No content changes were made. Signed 9/26/2017 Andrew D. Stern Date Director Analyze, Forecast, and Support Office NWSI 10-519 October 10, 2017 WFO Air Quality Products Specification Table of Contents: Page 1. Introduction 3 2. Air Quality Statement (AQI) 3 2.1 Mission Connection 3 2.2 Issuance Guidelines 3 2.2.1 Creation Software 3 2.2.2 Issuance Criteria 3 2.2.2.1 Routine Issuances 3 2.2.3 Issuance Time 4 2.2.4 Valid Time 4 2.2.5 Product Expiration Time 4 2.3 Technical Description 4 2.3.1 Universal Geographic Code (UGC) Type 4 2.3.2 Mass News Disseminator (MND) Broadcast Instruction Line 4 2.3.3 MND Product Type Line 4 2.3.4 Content 5 2.4 Updates and Corrections 5 3. Air Quality Alert Message (AQA) 5 3.1 Mission Connection 5 3.2 Issuance Guidelines 5 3.2.1 Creation Software 5 3.2.2 Issuance Criteria 5 3.2.2.1 Non-Routine Issuances 6 3.2.3 Issuance Time 6 3.2.4 Valid Time 6 3.2.5 Product Expiration Time 6 3.3 Technical Description 6 3.3.1 UGC Type 6 3.3.2 MND Broadcast Instruction Line 6 3.3.3 MND Product Type Line 6 3.3.4 Content 7 3.4 Updates and Corrections 7 APPENDIX – Product Examples and Air Quality Resources A-1 2 NWSI 10-519 October 10, 2017 1.