Health Effects from Sahara Dust Particles ETC/ACM
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Variability of Mineral Dust Deposition in the Western Mediterranean Basin and South-East of France
Atmos. Chem. Phys., 16, 8749–8766, 2016 www.atmos-chem-phys.net/16/8749/2016/ doi:10.5194/acp-16-8749-2016 © Author(s) 2016. CC Attribution 3.0 License. Variability of mineral dust deposition in the western Mediterranean basin and south-east of France Julie Vincent1, Benoit Laurent1, Rémi Losno1,a, Elisabeth Bon Nguyen1, Pierre Roullet2, Stéphane Sauvage3, Servanne Chevaillier1, Patrice Coddeville3, Noura Ouboulmane1, Alcide Giorgio di Sarra4, Antonio Tovar-Sánchez5,6, Damiano Sferlazzo4, Ana Massanet6, Sylvain Triquet1, Rafael Morales Baquero7, Michel Fornier8, Cyril Coursier9, Karine Desboeufs1, François Dulac10, and Gilles Bergametti1 1Laboratoire Interuniversitaire des Systèmes Atmosphériques (LISA), UMR7583 CNRS, Université Paris Denis Diderot, Université Paris-Est Créteil, Institut Pierre-Simon Laplace, Paris, France 2Ingénierie, Conseil, Assistance technique, Recherche, Étude (ICARE Ingénierie), Paris, France 3Département Sciences de l’Atmosphère et Génie de l’Environnement (SAGE), Mines Douai, 59508, Douai, France 4Laboratory for Earth Observations and Analyses (ENEA), Santa Maria di Galeria, Italy 5Andalusian Marine Science Institute (ICMAN, CSIC), Cádiz, Spain 6Institut Mediterrani d’Estudis Avançats (IMEDEA-CSIC/UIB), Balearic Island, Spain 7Departamento Ecologia, Universitad Granada, Granada, Spain 8Mediterranean Institute of Oceanography (MIO), UMR7294 CNRS, UMR235 IRD, Université Aix-Marseille, Université du Sud Toulon-Var, Marseille, France 9Parc national des Ecrins, Le Casset, France 10Laboratoire des Sciences du Climat et de l’Environnement (LSCE), UMR 8212 CEA-CNRS-UVSQ, Institut Pierre-Simon Laplace, Gif-sur-Yvette, France apresent address: Institut de Physique du Globe de Paris (IPGP), UMR7154 CNRS, Sorbonne Paris Cité, Université Paris Denis Diderot, Paris, France Correspondence to: J. Vincent ([email protected]) Received: 25 September 2015 – Published in Atmos. -
Proposal for Inclusion of the African Wild Ass (Eritrea)
CMS CONVENTION ON Distribution: General MIGRATORY UNEP/CMS/COP12/Doc.25.1.7(a) 9 June 2017 SPECIES Original: English 12th MEETING OF THE CONFERENCE OF THE PARTIES Manila, Philippines, 23 - 28 October 2017 Agenda Item 25.1 PROPOSAL FOR THE INCLUSION OF THE AFRICAN WILD ASS (Equus africanus) ON APPENDIX I AND II OF THE CONVENTION Summary: The Government of Eritrea has submitted the attached proposal* for the inclusion of the African Wild Ass (Equus africanus) on Appendix I and II of CMS. A proposal for the inclusion of the same taxon on Appendix I of CMS has been submitted independently by the Government of Ethiopia. The proposal is reproduced in document UNEP/CMS/COP12/Doc.25.1.7(b). *The geographical designations employed in this document do not imply the expression of any opinion whatsoever on the part of the CMS Secretariat (or the United Nations Environment Programme) concerning the legal status of any country, territory, or area, or concerning the delimitation of its frontiers or boundaries. The responsibility for the contents of the document rests exclusively with its author. UNEP/CMS/COP12/Doc.25.1.7(a) PROPOSAL FOR THE INCLUSION OF THE AFRICAN WILD ASS (Equus africanus) ON APPENDIX I AND II OF THE CONVENTION A. PROPOSAL Inclusion of all subspecies of African wild ass Equus africanus to Appendix I and Appendix II of the Convention on the Conservation of Migratory Species of Wild Animals: B. PROPONENT: ERITREA C. SUPPORTING STATEMENT 1. Taxonomy This proposal does not follow the current nomenclatural reference for terrestrial mammals adopted by CMS, i.e. -
The Question of 'Race' in the Pre-Colonial Southern Sahara
The Question of ‘Race’ in the Pre-colonial Southern Sahara BRUCE S. HALL One of the principle issues that divide people in the southern margins of the Sahara Desert is the issue of ‘race.’ Each of the countries that share this region, from Mauritania to Sudan, has experienced civil violence with racial overtones since achieving independence from colonial rule in the 1950s and 1960s. Today’s crisis in Western Sudan is only the latest example. However, very little academic attention has been paid to the issue of ‘race’ in the region, in large part because southern Saharan racial discourses do not correspond directly to the idea of ‘race’ in the West. For the outsider, local racial distinctions are often difficult to discern because somatic difference is not the only, and certainly not the most important, basis for racial identities. In this article, I focus on the development of pre-colonial ideas about ‘race’ in the Hodh, Azawad, and Niger Bend, which today are in Northern Mali and Western Mauritania. The article examines the evolving relationship between North and West Africans along this Sahelian borderland using the writings of Arab travellers, local chroniclers, as well as several specific documents that address the issue of the legitimacy of enslavement of different West African groups. Using primarily the Arabic writings of the Kunta, a politically ascendant Arab group in the area, the paper explores the extent to which discourses of ‘race’ served growing nomadic power. My argument is that during the nineteenth century, honorable lineages and genealogies came to play an increasingly important role as ideological buttresses to struggles for power amongst nomadic groups and in legitimising domination over sedentary communities. -
African Dust Carries Microbes Across the Ocean: Are They Affecting Human and Ecosystem Health?
African Dust Carries Microbes Across the Ocean: Are They Affecting Human and Ecosystem Health? Atmospheric transport of dust from northwest Africa to the western Atlantic Ocean region may be responsible for a number of environmental hazards, including the demise of Caribbean corals; red tides; amphibian diseases; increased occurrence of asthma in humans; and oxygen depletion ( eutro phication) in estuaries. Studies of satellite images suggest that hundreds of millions of tons of dust are trans ported annually at relatively low alti tudes across the Atlantic Ocean to the Caribbean Sea and southeastern United States. The dust emanates from the expanding Sahara/Sahel desert region in Africa and carries a wide variety of bacteria and fungi. The U.S. Geological Survey, in Figure 1. The satellite image, acquired by NASNGoddard Spaceflight Center's SeaWiFS Project and ORB IMAGE collaboration with the NASA/Goddard on February 26, 2000, shows one of the largest Saharan dust storms ever observed by SeaWiFS as it moves out Spaceflight Center, is conducting a study over the eastern Atlantic Ocean. Spain and Portugal are at the upper right Morocco is at the lower right. to identify microbes-bacteria, fungi , viruses-transported across the Atlantic in African soil dust. Each year, mil lions of tons of desert dust blow off the west Aftican coast and ride the trade winds across the ocean, affecting the entire Caribbean basin, as well as the southeastern United States. Of the dust reaching the U.S., Rorida receives about 50 percent, while tl1e rest may range as far nortl1 as Maine or as far west as Colorado. -
The Sahara – Europe's New Deadly External Border
The Sahara EUrope’s new deadly external border Edited by Andrea Stäritz and Julia Stier December 2018 A publication by borderline europe – Menschenrechte ohne Grenzen and Bildungswerk Berlin der Heinrich-Böll-Stiftung Photo: Christian Jakob The Sahara – EUrope’s new deadly external border The Sahara – EUrope’s new deadly external border Photo by: Andrea Stäritz Andrea Stäritz is a journalist and consultant focusing on West Africa since close to 20 years. After having worked in Index Nigeria for 5 years, she Preface returned to Berlin in the end of 2017 where she joined borderline -europe to pag.03 strengthen the work on the externalized borders in Africa. She has contributed to the Migration Control Preface Project of Tageszeitung from by Andrea Stäritz & Julia Stier West Africa and is now by Andrea Stäritz & Julia Stier focusing on human rights violations on the new In 1993, the German government ratified the rivers Oder and Neiße when these southern border of the the so-called ‘asylum compromise’, chan- rivers were still physical EU borders. European Union in Africa. ging the constitutional right to asylum. Today Agadez in Niger is considered the pag.04 pag.09 Consequently victims of civil war would virtual externalized border of the Europe- not have the right to asylum but would get an Union. European financial aid, techni- subsidiary protection with limited rights. cal devices, military check points and “Defending” EUropean The Sahara a cemetery This was never really applied and for the drone surveillance in the desert are the borders in the Sahara under the open sky Photo by: first time used more than 20 years later main pillars of an externalized EU border. -
Atmospheric Dust on Mars: a Review
47th International Conference on Environmental Systems ICES-2017-175 16-20 July 2017, Charleston, South Carolina Atmospheric Dust on Mars: A Review François Forget1 Laboratoire de Météorologie Dynamique (LMD/IPSL), Sorbonne Universités, UPMC Univ Paris 06, PSL Research University, Ecole Normale Supérieure, Université Paris-Saclay, Ecole Polytechnique, CNRS, Paris, France Luca Montabone2 Laboratoire de Météorologie Dynamique (LMD/IPSL), Paris, France & Space Science Institute, Boulder, CO, USA The Martian environment is characterized by airborne mineral dust extending between the surface and up to 80 km altitude. This dust plays a key role in the climate system and in the atmospheric variability. It is a significant issue for any system on the surface. The atmospheric dust content is highly variable in space and time. In the past 20 years, many investigations have been conducted to better understand the characteristics of the dust particles, their distribution and their variability. However, many unknowns remain. The occurrence of local, regional and global-scale dust storms are better documented and modeled, but they remain very difficult to predict. The vertical distribution of dust, characterized by detached layers exhibiting large diurnal and seasonal variations, remains quite enigmatic and very poorly modeled. Nomenclature Ls = Solar Longitude (°) MY = Martian year reff = Effective radius τ = Dust optical depth (or dust opacity) CDOD = Column Dust Optical Depth (i.e. τ integrated over the atmospheric column) IR = Infrared LDL = Low Dust Loading (season) HDL = High Dust Loading (season) MGS = Mars Global Surveyor (NASA spacecraft) MRO = Mars Reconnaissance Orbiter (NASA spacecraft) MEX = Mars Express (ESA spacecraft) TES = Thermal Emission Spectrometer (instrument aboard MGS) THEMIS = Thermal Emission Imaging System (instrument aboard NASA Mars Odyssey spacecraft) MCS = Mars Climate Sounder (instrument aboard MRO) PDS = Planetary Data System (NASA data archive) EDL = Entry, Descending, and Landing GCM = Global Climate Model I. -
Shankar Chellam, University of Houston (Currently at Texas A&M)
TO: Texas Air Research Center FROM: Shankar Chellam, University of Houston (currently at Texas A&M) SUBJECT: Final Report PROJECT NUMBER: 413UHH0143A PROJECT TITLE: Detailed elemental characterization of Saharan dust to quantify its contributions to PM2.5 and PM10 during episodic intrusions in Houston PROJECT PERIOD: September 1, 2013 – July 15, 2015 DATE: November 7, 2015 BACKGROUND The arid regions of North Africa are the world’s largest contributor of dust, estimated to emit about 800 Tgy-1 of soil dust annually. This North African particulate matter (PM) is transported across the Atlantic Ocean to the southern continental United States increasing the ambient PM10 and PM2.5 burden in Texas typically during the summer and early fall seasons. It is emphasized that isolating air pollutant contributions is difficult in complex urban environments. Also, the ability of detailed chemical speciation to differentiate sources is challenged because of the existence of myriad local sources. Another important source in Texas is primary emissions from motor vehicles. According to the United States Department of Transportation’s Federal Highway Administration, the State of Texas ranks second only to California in terms of vehicle miles traveled, with nearly 19 billion miles driven in November 2011 alone. Realistic estimates of tailpipe and non-tailpipe particulate emissions under actual on-road conditions incorporating several real-world sources of variability including maintenance histories, vehicle age, engine size and type, driving habits, and season can be obtained from measurements in roadway tunnels. We are interested in developing methods to quantify long-range transported PM as well as those locally emitted from motor vehicles. -
Cloud Icing by Mineral Dust and Impacts to Aviation Safety
www.nature.com/scientificreports OPEN Cloud icing by mineral dust and impacts to aviation safety Slobodan Nickovic1*, Bojan Cvetkovic1, Slavko Petković1, Vassilis Amiridis2, Goran Pejanović1, Stavros Solomos2,3, Eleni Marinou2,4 & Jugoslav Nikolic1 Ice particles in high-altitude cold clouds can obstruct aircraft functioning. Over the last 20 years, there have been more than 150 recorded cases with engine power-loss and damage caused by tiny cloud ice crystals, which are difcult to detect with aircraft radars. Herein, we examine two aircraft accidents for which icing linked to convective weather conditions has been ofcially reported as the most likely reason for catastrophic consequences. We analyze whether desert mineral dust, known to be very efcient ice nuclei and present along both aircraft routes, could further augment the icing process. Using numerical simulations performed by a coupled atmosphere-dust model with an included parameterization for ice nucleation triggered by dust aerosols, we show that the predicted ice particle number sharply increases at approximate locations and times of accidents where desert dust was brought by convective circulation to the upper troposphere. We propose a new icing parameter which, unlike existing icing indices, for the frst time includes in its calculation the predicted dust concentration. This study opens up the opportunity to use integrated atmospheric-dust forecasts as warnings for ice formation enhanced by mineral dust presence. Tere have been more than 150 accidents reported by commercial airplanes 1,2 related to cloud ice impacts, such as engine power loss, blade damage, and the icing of instrument sensors. Most of these incidences have been linked to icing in the upper troposphere in the vicinity of deep summer convection systems. -
Article Size Ery Year
Atmos. Chem. Phys., 18, 1023–1043, 2018 https://doi.org/10.5194/acp-18-1023-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 3.0 License. A detailed characterization of the Saharan dust collected during the Fennec campaign in 2011: in situ ground-based and laboratory measurements Adriana Rocha-Lima1,2, J. Vanderlei Martins1,3, Lorraine A. Remer1, Martin Todd4, John H. Marsham5,6, Sebastian Engelstaedter7, Claire L. Ryder8, Carolina Cavazos-Guerra9, Paulo Artaxo10, Peter Colarco2, and Richard Washington7 1University of Maryland, Baltimore County, Baltimore, MD, USA 2Atmospheric Chemistry and Dynamic Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, USA 3Climate and Radiation Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, USA 4Department of Geography, University of Sussex, Sussex, UK 5School of Earth and Environment, University of Leeds, Leeds, UK 6National Center for Atmospheric Science, Leeds, UK 7Climate Research Lab, Oxford University Center for the Environment, Oxford, UK 8Department of Meteorology, University of Reading, Reading, UK 9Institute for Advanced Sustainability Studies, Potsdam, Germany 10Instituto de Física, Universidade de São Paulo, São Paulo, Brazil Correspondence: Adriana Rocha-Lima ([email protected]) Received: 25 March 2017 – Discussion started: 20 June 2017 Revised: 14 November 2017 – Accepted: 7 December 2017 – Published: 26 January 2018 Abstract. Millions of tons of mineral dust are lifted by the atively high mean SSA of 0.995 at 670 nm was observed at wind from arid surfaces and transported around the globe ev- this site. The laboratory results show for the fine particle size ery year. The physical and chemical properties of the min- distributions (particles diameter < 5µm and mode diameter at eral dust are needed to better constrain remote sensing ob- 2–3 µm) in both sites a spectral dependence of the imaginary servations and are of fundamental importance for the under- part of the refractive index Im.m/ with a bow-like shape, standing of dust atmospheric processes. -
The Hot Arctic and Cold Sahara Imagine Eskimos Living in the Desert
The Hot Arctic and Cold Sahara Imagine Eskimos living in the desert or Africans calling the North Pole their home. Now that sounds absolutely ridiculous but what if the world had turned itself upside down and this was the reality? Would they be able to survive? Perhaps they would. These places have extreme weather conditions and people have survived extremely hot and intensively cold days so perhaps living in a completely opposite extreme climate isn’t that hard after all. All they have to do is switch their mode of thinking from either bitter cold to hot or from blazing hot to cold. If they continue to live by the basic needs of life, then survival in either climate would be a synch. The Inuit up in Northern Canada use caribou and wolverine fur coats to shield them from bitter icy cold winds of the Arctic. They use seal leather boots to keep their feet warm while walking on the hard icy grounds of the cold desert and if they encounter a snow storm, they don’t have to worry about getting a frost bite from wet shoes. Traveling across the globe to the Algerians living in the Sahara desert, these people also need to protect themselves, but this time, it’s from the scorching hot equatorial sun. Covering their entire body with a lose cotton garment is important to keep cool. But it’s pretty ironic that even the people of the hot climate have to cover their heads with a type of turban commonly called a howli . The attire and fashion in both regions are definitely starting to seem like they have a direct connection with each other. -
Saharan Dust Composition on the Way to the Americas and Potential Impacts on Atmosphere and Biosphere
1 Saharan dust composition on the way to the Americas and potential impacts on atmosphere and biosphere K. Kandler Institut für Angewandte Geowissenschaften, Technische Universität Darmstadt, 64287 Darmstadt, Germany The Saharan dust plume 2 over the Western Atlantic Ocean K. Kandler: Zum Einfluss des SaharastaubsKarayampudi et auf al., 1999, das doi : Klima10.1175/1520 – -Erkenntnise0477(1999)080 aus dem Saharan Mineral Dust Experiment (SAMUM) The Saharan dust plume 3 on its arrival overover the the Caribbean Western Atlantic Ocean PR daily averaged surface dust concentration (in µg-3), modelled for 23 June 1993 Kallos et al. 2006, doi: 10.1029/2005JD006207 K. Kandler: Zum Einfluss des SaharastaubsKarayampudi et auf al., 1999, das doi : Klima10.1175/1520 – -Erkenntnise0477(1999)080 aus dem Saharan Mineral Dust Experiment (SAMUM) Case study of a dust event 4 from Bodélé depression reaching South America daily lidar scans starting Feb 19, 2008 from Ben-Ami et al. 2010 doi: 10.5194/acp-10-7533-2010 5 Dust composition and its dependencies, interaction and potential impacts DEPOSITION TRANSPORT EMISSION terrestrial solar radiative impact wet processing radiative impact photochemistry cloud impact indirect radiative impact anthropogeneous/ biomass burning aerosol admixture heterogeneous chemistry dry removal sea-salt interaction wet removal terrestrial geological basement ecosystem impact type of weathering surface transport human/plant/animal marine ecosystem impact health issues chemical processing emission meteorology 6 Implications for -
Analysis of Dust Aerosol Retrievals Using Satellite Data in Central Asia
Article Analysis of Dust Aerosol Retrievals Using Satellite Data in Central Asia Longlei Li * and Irina N. Sokolik School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA 30332, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-404-754-1177 Received: 8 June 2018; Accepted: 19 July 2018; Published: 24 July 2018 Abstract: Several long-term monitoring of aerosol datasets from the Moderate Resolution Imaging Spectroradiometer (MODIS) on board Terra/Aqua, Multi-angle Imaging SpectroRadiometer (MISR), Sea-Viewing Wide Field-of-View Sensor (SeaWiFS) were used to derive the dust aerosol optical depth (DOD) in Central Asia based on the Angstrom exponent parameter and/or the particle shape. All sensors agree very well on the interannual variability of DOD. The seasonal analysis of DOD and dust occurrences identified the largest dust loading and the most frequent dust occurrence in the spring and summer, respectively. No significant trend was found during the research period in terms of both DOD and the dust occurrence. Further analysis of Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) aerosol products on a case-by-case basis in most dust months of 2007 suggested that the vertical structure is varying in terms of the extension and the dust loading from one event to another, although dust particles of most episodes have similar physical characteristics (particle shape and size). Our analysis on the vertical structure of dust plumes, the layer-integrated color ratio and depolarization ratio indicates a varied climate effect (e.g., the direct radiative impact) by mineral dust, dependent on the event being observed in Central Asia.