Key Points in Air Pollution Meteorology
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Numerical Study of Winter Shamal Wind Forcing on the Surface Current and Wave Field in Bushehr's Offshore Using MIKE21
INTERNATIONAL JOURNAL OF COASTAL & OFFSHORE ENGINEERING IJCOE Vol.2/No. 2/Summer 2018 (57-65) Available online at: http://ijcoe.org/browse.php?a_code=A-10-171-2&sid=1&slc_lang=en Numerical Study of Winter Shamal Wind Forcing on the Surface Current and Wave Field in Bushehr's Offshore Using MIKE21 Mohammad Pakhirehzan1, Maryam Rahbani2*, Hossein Malakooti3 1 Ph.D. student, Faculty of Marine Science and Technology, University of Hormozgan, Bandar Abbas, IRAN; [email protected] 2* Assistant Prof., Faculty of Marine Science and Technology, University of Hormozgan, Bandar Abbas, IRAN; [email protected] 3 Associate Prof., Faculty of Marine Science and Technology, University of Hormozgan, Bandar Abbas, IRAN; [email protected] ARTICLE INFO ABSTRACT Article History: Marine areas are affected by different atmospheric phenomena such as wind Received: 11 Jun. 2018 and storm. In this research the effect of a large scale atmospheric phenomenon, Accepted: 18 Sep. 2018 known as Winter Shamal Wind, is investigated on the regime of currents and waves in the northwest part of the Persian Gulf. This wind normally occurs for Keywords: the period of three to seven days, during December to early March. MIKE21 Persian Gulf Coupled Model FM was applied to study the pattern of current and waves for winter Shamal wind MIKE21 this period. To provide the hydrodynamic data for the model and validate the simulated results, the wind data of ECMWF and mast meteorology of coastal synoptic station of Bushehr and wave data of buoy located offshore of Bushehr was used. The results indicated only a slight increase in current speed with no significant change in current direction during Winter Shamal Wind, showing a stable current pattern in northwest of the Persian Gulf. -
Analysis of the Long-Term Variability of Poor Visibility Events in the UAE and the Link with Climate Dynamics
atmosphere Article Analysis of the Long-Term Variability of Poor Visibility Events in the UAE and the Link with Climate Dynamics Amal Aldababseh * and Marouane Temimi Chemical and Environmental Engineering Department, Masdar Institute of Science and Technology, Khalifa University of Science and Technology, Masdar City, P.O. Box 54224, Abu Dhabi, UAE; [email protected] * Correspondence: [email protected] Received: 22 October 2017; Accepted: 28 November 2017; Published: 4 December 2017 Abstract: The goal of this study is to investigate the variability of poor visibility events occurring hourly in the UAE and their relationship to climate dynamics. Hourly visibility observation data spanning more than three decades from ten stations across the country were used. Four intervals of low visibility, between 0.10 km and 5.0 km, were considered. Poor visibility records were analyzed under wet and dry weather conditions. The Mann–Kendall test was used to assess the inferred trends of low visibility records. The relationships between poor visibility measurements and associated meteorological variables and climate oscillations were also investigated. Results show that Fujairah city has the highest average visibility values under wet weather conditions, while Abu Dhabi city has the lowest average visibility values under both wet and dry conditions. Wet weather conditions had a greater impact than dry weather conditions on visibility deterioration in seven out of the ten stations. Results confirm that fog and dust contribute significantly to the deterioration of visibility in the UAE and that Abu Dhabi has been more impacted by those events than Dubai. Furthermore, the numbers of fog and dust events show steep increasing trends for both cities. -
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. -
Coniglio Et Al. (2006)
P1.30 FORECASTING THE SPEED AND LONGEVITY OF SEVERE MESOSCALE CONVECTIVE SYSTEMS Michael C. Coniglio∗1 and Stephen F. Corfidi2 1NOAA/National Severe Storms Laboratory, Norman, OK 2NOAA/Storm Prediction Center, Norman, OK 1. INTRODUCTION b. MCS maintenance Forecasting the details of mesoscale convective Predicting MCS maintenance is fraught with systems (MCSs) (Zipser 1982) continues to be a difficult challenges such as understanding how deep convection problem. Recent advances in numerical weather is sustained through system/environment interactions prediction models and computing power have allowed (Weisman and Rotunno 2004, Coniglio et al. 2004b, for explicit real-time prediction of MCSs over the past Coniglio et al. 2005), how pre-existing mesoscale few years, some of which have supported field features influence the system (Fritsch and Forbes 2001, programs (Davis et al. 2004) and collaborative Trier and Davis 2005), and how the disturbances experiments between researchers and forecasters at generated by the system itself can alter the system the Storm Prediction Center (SPC) (Kain et al. 2005). structure and longevity (Parker and Johnson 2004c). While these numerical forecasts of MCSs are promising, the utility of these forecasts and how to best use the From an observational perspective, Evans and capabilities of the high-resolution models in support of Doswell (2001) suggest that the strength of the mean operations is unclear, especially from the perspective of wind (0-6 km) and its effects on cold pool development the Storm Prediction Center (SPC) (Kain et al. 2005). and MCS motion play a significant role in sustaining Therefore, refining our knowledge of the interactions of long-lived forward-propagating MCSs that produce MCSs with their environment remains central to damaging surface winds (derechos) through modifying advancing our near-term ability to forecast MCSs. -
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. -
Dust Transport Over the Arabian Peninsula and Kuwait
Dust Transport over the Arabian Peninsula and Kuwait Carly Baumann1* Olga Kalashnikova2 Michael Garay2 Jun Wang1 1 University of Nebraska – Lincoln 2 Jet Propulsion Lab, Pasadena, CA Case 1: MarCh 2012 I. IntroduCDon and BaCkground Surface and METAR data Satellite images, parKcularly those showing significant amounts of MODIS Meteosat Visibility During Dust Event Acknowledgments dust in the atmosphere, are examined to find the source of dust March 16-21, 2012, MODIS images have a wider swath enabling be=er viewing of the dust event PM10 Models 12 events, determine meteorological parameters for a severe versus 10 Kalashnikova, Olga, for METAR report and Meteosat 8 images insignificant dust event, and determine velocity, direcKon, and 6 height of dust storms to see what other regions are affected. Vis (km) 4 Garay, Michael, and Nelson, David for usage with MINX 2 Linkages between dust plume informaon at the source and dust 0 Wang, Jun for PM10 models properKes in downwind transport regions were evaluated using 0 50 100 150 200 250 This project was funded by JPLSIP (summer 2012) and March 17, 2012 04:30 16/03/12 to 07:00 20/03/12 (30 minute intervals) Space Grant at the Jet Propulsion Lab and California the MINX somware applicaon. Images from the MISR instrument March 17, 2012 Using the same method as on Meteosat the distance was 220,206 m over 6 hours aboard NASA’s Terra satellite were brought into MINX and height Distance between both points = 222,719 m (Google Earth) over 6.5 hours Dust traveling at 10.1 ms-1 START: March 17, 2012 06:30Z END: March 19, 2012 15:00Z InsKtute of Technology in Pasadena, CA. -
Risk Warning and Crisis Management for Dust Storm Effects on Western Border of Iran Rapid Response Mapping for Dust Storm Crisis
United Nations International Conference on Space-based Technologies for Disaster Risk Management “Best Practices for Risk Reduction and Rapid Response Mapping” Beijing, China, 22-25 November 2011 Risk Warning and Crisis Management for Dust Storm Effects on Western border of Iran Rapid Response mapping for Dust Storm Crisis M. Morabbi Mahdasht Satellite Receiving Station, Alborz Space Center Iranian Space Agency(ISA) [email protected] United Nations International Conference on Space-based Technologies for Disaster Risk Management “Best Practices for Risk Reduction and Rapid Response Mapping” Beijing, China, 22-25 November 2011 Geographic Setting: United Nations International Conference on Space-based Technologies for Disaster Risk Management “Best Practices for Risk Reduction and Rapid Response Mapping” Beijing, China, 22-25 November 2011 Geographic Setting: IR. Iran Position in south-west Asia 44° 02′ E and 63° 20′ E eastern longitude 25° 03′ N to 39° 46′ N northern latitude Area : about 1.648 million sq km Borders: Azerbaijan, Turkmenistan and Armenia in the north, which are around the Caspian Sea, Afghanistan and Pakistan in the east ; Turkey and Iraq in the west. Persian Gulf and Oman Sea in the south Natural Disaster & IR. Iran Due to its climatological and environmental diversity, the country has long been marked as a disaster-prone territory. Moreover, it has been facing man-made disasters, mainly due to the poor political, social and economic stability in its neighboring countries which in turn lead to further natural disasters caused by natural degradation. During recent decades, the country has been facing numerous large scale natural disasters as dust storm. -
1 Mesoscale Meteorology: Density Currents 11 April 2017 Introduction
Mesoscale Meteorology: Density Currents 11 April 2017 Introduction A density current is defined as the intrusion of a denser fluid beneath a lighter fluid. Consider the hydrostatic equation: ∂p = −ρg ∂z Let us consider a density current of finite depth, such that isobaric surfaces are parallel to constant height surfaces above the density current. Evaluated between the ground (z = 0) and the top of the density current, the denser fluid will have a larger decrease in pressure over the depth of the density current than the lighter fluid. For fixed pressure at the top of the density current, this implies the presence of a mesohigh at the surface within the density fluid. (This is the same as a hypsometric argument, where a colder layer is associated with reduced thickness and thus higher pressure below the layer.) This establishes a horizontal pressure gradient force directed away from the mesohigh that is responsible for density current motion and displacing the lighter fluid above the denser fluid. While much of the pressure differential across a density current results from the above hydrostatic principles, there are substantial non-hydrostatic contributions along the leading edge of the density current and within the density current beneath the strongest downdraft. Further, a wake low, which forms due to compressional warming associated with unsaturated descent atop the density current, may be found rearward of the mesohigh. In such a case, the horizontal pressure gradient force in the rear of a density current may be elevated over that along the leading edge. Like sea breezes, which are a subclass of density current, density currents typically have a head on their leading edge, with depth that can be as much as twice as large as that behind its leading edge. -
Using High-Resolution WRF Model Simulations to Investigate The
y & W log ea to th a e im r l F C o f r Alsarraf and Van Den Broeke, J Climatol Weather Forecasting 2015, 3:1 e o Journal of c l a a s n t r i n DOI: 10.4172/2332-2594.1000126 u g o J ISSN: 2332-2594 Climatology & Weather Forecasting Research Article Article OpenOpen Access Access Using High-Resolution WRF Model Simulations to Investigate the Relationship between Mesoscale Circulations and Aerosol Transport over Kuwait Hussain Alsarraf 1* and Matthew Van Den Broeke2 1Kuwait Meteorological department, Kuwait 2Department of Earth and Atmospheric Sciences, University of Nebraska – Lincoln, USA Abstract Two case studies have been investigated using high-resolution WRF model simulations. The purpose of these case studies is to determine the effects of wind patterns on visibility and aerosol transport in the region. In the first case study, strong synoptic-scale forcing led to a large-scale pressure gradient resulting in strong wind and long- range aerosol transport. In the second case study, the mesoscale land/sea breeze offset weak synoptic-scale forcing near the coast. The daytime sea breeze and nighttime land breeze limited the ventilation of air masses and allowed recirculation of contaminants and aerosols near the shoreline, which may strongly influence visibility and air quality locally. Keywords: WRF; Synoptic scale forcing; Mesoscale circulation; In other cases, the Shamal wind can be caused by a dry cold Aerosol transport; Visibility; Arabian peninsula; Shamal; Sea breeze; front crossing the Arabian Peninsula, which reduces the maximum Air quality temperature [2]. July is persistently dry and hot, with temperatures that can reach nearly 50°C. -
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. -
Poverty Rates
Public Disclosure Authorized Public Disclosure Authorized Public Disclosure Authorized Public Disclosure Authorized Mapping Poverty inIraq Mapping Poverty Where are Iraq’s Poor: Poor: Iraq’s are Where Acknowledgements This work was led by Tara Vishwanath (Lead Economist, GPVDR) with a core team comprising Dhiraj Sharma (ETC, GPVDR), Nandini Krishnan (Senior Economist, GPVDR), and Brian Blankespoor (Environment Specialist, DECCT). We are grateful to Dr. Mehdi Al-Alak (Chair of the Poverty Reduction Strategy High Committee and Deputy Minister of Planning), Ms. Najla Ali Murad (Executive General Manager of the Poverty Reduction Strategy), Mr. Serwan Mohamed (Director, KRSO), and Mr. Qusay Raoof Abdulfatah (Liv- ing Conditions Statistics Director, CSO) for their commitment and dedication to the project. We also acknowledge the contribution on the draft report of the members of Poverty Technical High Committee of the Government of Iraq, representatives from academic institutions, the Ministry of Planning, Education and Social Affairs, and colleagues from the Central Statistics Office and the Kurdistan Region Statistics during the Beirut workshop in October 2014. We are thankful to our peer reviewers - Kenneth Simler (Senior Economist, GPVDR) and Nobuo Yoshida (Senior Economist, GPVDR) – for their valuable comments. Finally, we acknowledge the support of TACBF Trust Fund for financing a significant part of the work and the support and encouragement of Ferid Belhaj (Country Director, MNC02), Robert Bou Jaoude (Country Manager, MNCIQ), and Pilar -
Al Iraqi 1969 Baghdad College, Baghdad, Iraq All Physical Materials Associated with the New England Province Archive Are Currently Held by the Jesuit Archives in St
New England Jesuit Archives are located at Jesuit Archives (St. Louis, MO) Digitized Collections hosted by CrossWorks. Baghdad College Yearbook 1969 Al Iraqi 1969 Baghdad College, Baghdad, Iraq All physical materials associated with the New England Province Archive are currently held by the Jesuit Archives in St. Louis, MO. Any inquiries about these materials should be directed to the Jesuit Archives (http://jesuitarchives.org/). Electronic versions of some items and the descriptions and finding aids to the Archives, which are hosted in CrossWorks, are provided only as a courtesy. Digitized Record Information Baghdad College, Baghdad, Iraq, "Al Iraqi 1969" (1969). Baghdad College Yearbook. 29. https://crossworks.holycross.edu/baghdadcoll/29 The Arabesque cover design is from a sixteenth-century decoration of the Holy Qur'an. Photo by MAJID RASSAM, SD PUBLISHED BY THE OF BAGHDAD COLLEGE BAGHDAD IRAQ FOR THE PAST THIRTY-SEVEN YEARS BAGHDAD COLLEGE HAS BEEN PRIVILEGED TO PARTICIPATE IN THE EDUCATION OF IRAQI YOUTH. THE WORDS CHOSEN BY ITS FOUNDERS, MosT REVEREND WILLIAM A. RICE, s.J., AND REv. EDWARD F. MADARAS, S.J., TO DESCRIBE THE CoLLEGE WERE: "AN IRAQI ScHooL FOR IRAQI BoYs". THE EDUCATION OF YOUTH PRESENTS A CONTINUAL CHALLENGE TO THOSE ENGAGED IN THE TEACHING PROFESSION. THE INDIVIDUALS WHO ACCEPT THIS CHALLENGE SHOULD HAVE A UNIQUE SENSE OF DEDI CATION, OF UNDERSTANDING, AND OF GENEROSITY. FOR THEM, TEACHING IS MUCH MORE THAN A MERE JOB TO BE DONE. IT IS THEIR LIFE. IT IS WITH A DEEP SENSE OF GRATITUDE THAT WE DEDICATE THIS ISSUE OF "AL-IRAQI" TO THE IRAQI jESUIT FATHERS AND TO THE IRAQI TEACHERS AND STAFF, PAST AND PRESENT, OF BAGHDAD COLLEGE.