The Effect of Land Cover on the Air and Surface Urban Heat Island of a Desert Oasis

Total Page:16

File Type:pdf, Size:1020Kb

The Effect of Land Cover on the Air and Surface Urban Heat Island of a Desert Oasis Durham E-Theses The Eect of Land Cover on the Air and Surface Urban Heat Island of a Desert Oasis AL-ALI, ABDULRAHMAN,MUBARAK,H How to cite: AL-ALI, ABDULRAHMAN,MUBARAK,H (2015) The Eect of Land Cover on the Air and Surface Urban Heat Island of a Desert Oasis , Durham theses, Durham University. Available at Durham E-Theses Online: http://etheses.dur.ac.uk/11290/ Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in Durham E-Theses • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full Durham E-Theses policy for further details. Academic Support Oce, Durham University, University Oce, Old Elvet, Durham DH1 3HP e-mail: [email protected] Tel: +44 0191 334 6107 http://etheses.dur.ac.uk 2 The Effect of Land Cover on the Air and Surface Urban Heat Island of a Desert Oasis Submitted for the degree of Doctor of Philosophy Submitted by Abdulrahman Mubarak H. Al Ali Department of Geography Durham University United Kingdom June 2015 The Effect of Land Cover on the Air and Surface Urban Heat Island of a Desert Oasis Abdulrahman Mubarak H. Al Ali Abstract Cities often experience a distinct climate compared to the surrounding area characterized by differences in air temperature, humidity, wind speed and direction, and amount of precipitation. Thus far, research on the urban heat island (UHI) effect has focused on cool temperate, Mediterranean and tropical climatic regions, whereas less attention has been given to the study of arid regions where the daytime surface temperature can be extremely high. This study concerns the Al Ahsa oasis, Saudi Arabia, which is a rapidly developing urban centre in an arid region. The aim of this study is to analyze the effect of land cover on the urban and sub-urban environment using ground data and multi-scale and multi-temporal satellite thermal imagery. Land surface temperatures derived from satellite thermal imagery are compared with observations from ground-based fixed and mobile temperature and relative humidity logging stations for periods in February and July. Thermal radiometers from different sensors, Landsat 7 ETM+ and MODIS, were used to measure the outgoing radiation budget at specific locations within the urban landscape. Fieldwork was undertaken contemporary with satellite overpasses to measure the diurnal air temperatures and relative humidity across different land cover types including agriculture, urban, water, exposed rock surfaces, sabkha and sand dunes. These data provide the most complete experiment so far conducted to test and refine models of the thermal radiation budget of the arid zone at the sub-city scale. The findings of this study have emphasized the effectiveness of combining the two methods, ground and satellite data, to investigate the relationship between land cover and UHI intensity. Results reveal a significant relationship between UHI spatial distribution and land cover using the two methods: mobile traverses and remote sensing. The UHI intensity is higher during the summer than the winter and at night-time than in the day. The highest UHI intensity, (10.5 °C), is located over the two major cities in the oasis (Al Hufuf and Al Mubarraz) while the lowest temperatures (- 6.4 °C below UHI), are recorded in the small villages and vegetated areas during summer at night. The outcome of this thesis will help future urban development and planning projects and provide a framework for implementing rules and regulations by local government agencies for a sustainable urban development approach. Table of Contents TABLE OF CONTENTS i LIST OF ILLUSTRATIONS vii DECLARATION xvii ACKNOWLEDGEMENTS xviii Chapter 1: Introduction ...................................................................................................... 1 1.1 Applied Climatology and Urban Climate ................................................................ 1 1.2 Urban Heat Islands ................................................................................................... 2 1.2.1 Definition and Background .............................................................................. 2 1.2.2 Types of Urban Heat Islands ............................................................................ 4 1.2.2.1 Surface Urban Heat Islands ...................................................................... 4 1.2.2.2 Atmospheric Urban Heat Islands .............................................................. 5 1.3 Microclimates and the Urban Heat Island ............................................................... 6 1.3.1 The formation of urban heat islands................................................................. 8 1.3.1.1 Reduced vegetation cover in urban areas ................................................. 8 1.3.1.2 Properties of urban materials .................................................................... 9 1.3.1.3 Urban geometry ...................................................................................... 10 1.3.1.4 Radiation and energy budget .................................................................. 11 1.3.1.4.1 Short-wave radiation ............................................................................ 11 1.3.1.4.2 Thermal storage ................................................................................... 12 1.3.1.5 Anthropogenic heat ................................................................................. 13 1.3.1.6 Weather conditions and geographical location ....................................... 13 1.4 Measuring Urban Heat Islands............................................................................... 14 1.4.1 Ground Data Applications.............................................................................. 14 i 1.4.2 Remote Sensing Applications ........................................................................ 18 1.5 Significance of this Research ................................................................................. 24 1.5.1 Global Warming ............................................................................................. 24 1.5.2 Land Cover Change........................................................................................ 25 1.5.3 Energy Use ..................................................................................................... 26 1.5.4 Air Quality ..................................................................................................... 27 1.5.5 Human Health and Comfort ........................................................................... 28 1.5.6 Water Quality ................................................................................................. 29 1.6 Research Questions, Aims and Objectives ............................................................ 29 1.6.1 Research Questions ........................................................................................ 29 1.6.2 The Aim ......................................................................................................... 30 1.6.3 The Research Objectives ................................................................................ 30 1.7 Thesis Structure ..................................................................................................... 30 Chapter 2: Description of the Study Area ....................................................................... 32 2.1 Introduction ............................................................................................................ 32 2.2 Geographical location and background ................................................................. 32 2.3 Topography ............................................................................................................ 36 2.3.1 Aeolian formations ......................................................................................... 36 2.3.2 Sabkha deposits .............................................................................................. 37 2.3.3 Gravel deposits ............................................................................................... 38 2.3.4 Hills and Mesas .............................................................................................. 38 2.4 Local Climate ......................................................................................................... 38 2.4.1 Air Temperature ............................................................................................. 39 2.4.1.1 Summer and winter temperatures ........................................................... 39 2.4.1.2 Spring and autumn temperatures ............................................................ 40 2.4.1.3 Relative humidity .................................................................................... 41 2.4.1.4 Synoptic systems and wind patterns in the study area ............................ 41 ii 2.4.1.4.1 Pressure systems and winds in the winter ............................................ 42 2.4.1.4.2 Pressure systems and winds in the summer ......................................... 43 2.4.2 Rainfall ........................................................................................................... 44 2.5 Population
Recommended publications
  • Sand Dune Systems in Iran - Distribution and Activity
    Sand Dune Systems in Iran - Distribution and Activity. Wind Regimes, Spatial and Temporal Variations of the Aeolian Sediment Transport in Sistan Plain (East Iran) Dissertation Thesis Submitted for obtaining the degree of Doctor of Natural Science (Dr. rer. nat.) i to the Fachbereich Geographie Philipps-Universität Marburg by M.Sc. Hamidreza Abbasi Marburg, December 2019 Supervisor: Prof. Dr. Christian Opp Physical Geography Faculty of Geography Phillipps-Universität Marburg ii To my wife and my son (Hamoun) iii A picture of the rock painting in the Golpayegan Mountains, my city in Isfahan province of Iran, it is written in the Sassanid Pahlavi line about 2000 years ago: “Preserve three things; water, fire, and soil” Translated by: Prof. Dr. Rasoul Bashash, Photo: Mohammad Naserifard, winter 2004. Declaration by the Author I declared that this thesis is composed of my original work, and contains no material previously published or written by another person except where due reference has been made in the text. I have clearly stated the contribution by others to jointly-authored works that I have included in my thesis. Hamidreza Abbasi iv List of Contents Abstract ................................................................................................................................................. 1 1. General Introduction ........................................................................................................................ 7 1.1 Introduction and justification ........................................................................................................
    [Show full text]
  • Middle-To-Late-Pleistocene.Pdf
    Quaternary International 382 (2015) 200e214 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint Middle to Late Pleistocene human habitation in the western Nefud Desert, Saudi Arabia * Eleanor M.L. Scerri a, , Paul S. Breeze b, Ash Parton c, Huw S. Groucutt c, Tom S. White c, Christopher Stimpson c, Laine Clark-Balzan c, Richard Jennings c, Abdullah Alsharekh d, Michael D. Petraglia c a PACEA, University of Bordeaux, UMR 5199 Batiment^ B8, Allee Geoffrey St Hilaire, CS 50023, 33615 Pessac Cedex, France b Department of Geography, King's College London, K4U.06 Strand Campus, London WC2R 2LS, United Kingdom c School of Archaeology, Research Laboratory for Archaeology and the History of Art, University of Oxford, 28 New Barnett House, Little Clarendon Street, Oxford OX1 2HU, United Kingdom d Department of Archaeology, King Saud University, P.O. Box 2627, Riyadh 12372, Saudi Arabia article info abstract Article history: The Nefud Desert is crucial for resolving debates concerning hominin demography and behaviour in Available online 8 October 2014 the Saharo-Arabian belt. Situated at the interface between the Mediterranean Westerlies and African Monsoonal climate systems, the Nefud lies at the centre of the arid zone crossed by Homo sapiens Keywords: dispersing into Eurasia and the edges of the southernmost known extent of the Neanderthal range. In Pleistocene Palaeoenvironments 2013, the Palaeodeserts Project conducted an intensive survey of the western Nefud, to: (1) evaluate Lower Palaeolithic Pleistocene population dynamics in this important region of the Saharo-Arabian belt and (2) Middle Palaeolithic contribute towards understanding early modern human range expansions and interactions between different hominin species.
    [Show full text]
  • The Environmental History and Present Condition of Saudi Arabia's
    UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY The environmental history and present condition of Saudi Arabia's northern sand seas by J. W. Whitney I/, D. J. Faulkender, and Meyer Rubin 2/ Open-File Report 83- 7V Prepared for Ministry of Petroleum and Mineral Resources, Deputy Ministry for Mineral Resources Jiddah, Kingdom of Saudi Arabia This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature I/ U.S. Geological Survey, Denver, CO 80225 2/ U.S. Geological Survey, Radiocarbon Lab., Reston, VA 22092 1983 CONTENTS Page ABSTRACT................................................ 1 INTRODUCTION............................................ 2 PHYSICAL SETTING AND SEDIMENT SOURCES OF THE SAND SEAS.. 4 AGE AND ORIGIN OF THE SAND SEAS......................... 8 QUATERNARY EOLIAN AND LACUSTRINE DEPOSITS............... 12 Dune systems........................................ 12 Active versus stable dunes.......................... 15 Pleistocene and Holocene lake deposits.............. 18 Diatomite........................................... 24 PRESENT CONDITION OF THE SAND SEAS...................... 25 Precipitation and temperature....................... 25 Vegetation.......................................... 27 Modern and paleo-wind systems....................... 29 ENVIRONMENTAL HISTORY OF THE SAND SEAS.................. 32 DATA STORAGE............................................ 35 REFERENCES CITED........................................ 36 ILLUSTRATIONS
    [Show full text]
  • Saudi-Arabia
    Saudi-Arabia Last updated: 31-01-2004 Location and area Saudi Arabia is a monarchy of the Middle East, occupying most of the Arabian Peninsula, and bordered on the north by Jordan, Iraq, and Kuwait, on the east by the Persian Gulf and Qatar, on the southeast by the United Arab Emirates and Oman, on the south by the Republic of Yemen and on the west by the Red Sea and the Gulf of Aqaba. Boundaries in the southeast are not precisely defined. Saudi Arabia has an area of about 2,240,000 km2. (Microsoft Encarta Encyclopedia 2002). Topography Considerably more than half the area of Saudi Arabia is desert. Rub‘ al Khali, known as the Great Sandy Desert and as the "Empty Quarter", extends over much of the south-east and beyond the southern frontier. Largely unexplored, Rub‘ al Khali has an estimated area of about 777,000 km2. An extension of the Syrian Desert projects into northern Saudi Arabia, and extending southeast from this region is An Nafud, an upland desert of red sand covering an area of about 57,000 km2. Ad Dahna’, a narrow extension of this desert, links An Nafud and Rub‘ al Khali. A central plateau region, broken in the east by a series of uplifts, extends south from An Nafud. Several wadis (watercourses), dry except in the rainy season, traverse the plateau region. The western limits of the latter are delineated by a mountain range extending generally northwest and southeast along the eastern edge of Al hijāz and Asir regions. (Microsoft Encarta Encyclopedia 2002).
    [Show full text]
  • Climate and Vegetation • Most of Southwest Asia Has a Very Arid Climate
    Main Ideas Climate and Vegetation • Most of Southwest Asia has a very arid climate. • Irrigation is critical to growing crops in this very dry region. Places & Terms Rub al-Khali oasis A HUMAN PERSPECTIVE In the spring of 1999, three Canadian explor- salt flat ers retraced the steps of Sir Wilfred Thesiger’s 1946 epic journey across the Rub al-Khali on the Arabian Peninsula. It is one of the most extreme Connect to the Issues deserts in the world. Like Sir Wilfred, they crossed using camels, not population relocation four-wheel drive vehicles. But unlike Sir Wilfred, the Canadians were The climate of Southwest Asia equipped with late 20th-century explorers’ tools—personal location limits interaction between beacons, a satellite phone for communications, and laptop computers countries in the region. for recording details of the journey. Crossing this great arid expanse was physically challenging and took 40 days to complete. But for many of the region’s inhabitants, survival in the lands of this region is a chal- lenge every day. Variety in Arid Lands MOVEMENT A Bedouin caravan Southwest Asia is extremely arid. Most areas receive less than 18 inch- crosses a dry, rocky desert in es of precipitation a year. A huge portion of its land area is covered with Judea, a part of Israel. rough, dry terrain that varies from huge tracts of sand dunes to great How do conditions in the desert restrict movement? salt flats. Study the Map Skills on page 494 to learn more about desert vegetation. Because the region is so dry, its rivers do not flow year round.
    [Show full text]
  • An Analysis of the Differences Between Two Seasonal Saudi Arabian Dust Storms Using WRF-Chem
    University of Nevada, Reno An Analysis of the Differences Between Two Seasonal Saudi Arabian Dust Storms Using WRF-Chem A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Atmospheric Science by Yazeed Alsubhi Dr. Eric M. Wilcox/Thesis Advisor May, 2016 THE GRADUATE SCHOOL We recommend that the thesis prepared under our supervision by YAZEED ALSUBHI Entitled An Analysis of the Differences Between Two Seasonal Saudi Arabian Dust Storms Using WRF-Chem be accepted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Eric M. Wilcox, Ph.D., Advisor Michael Kaplan, Ph.D., Committee Member Mae Gustin, Ph.D., Graduate School Representative David W. Zeh, Ph.D., Dean, Graduate School May, 2016 i ABSTRACT This research focused on understanding the difference atmospheric conditions between two major dust storms in Saudi Arabia. These two types of dust storms occur annually over Saudi Arabia with different seasons, sources, and atmospheric dynamics. We analyzed the Sharav case study in the spring season from 31 March 2015 and the Shamal case study in the early summer season from 09 to 10 June 2015 using the HYSPLIT (Hybrid Single Particle Lagrangian Integrated Trajectory) model to determine the dust source regions and the MERRA (Modern Era-Retrospective Analysis for Research and Applications) data for the large-scale analyses. Dust particles are generated from the Sahara Desert in the Sharav case; however, these particles are generated from the Syrian and Iraqi Deserts in the Shamal case. The large-scale analyses show that the differences in the circulation over much of the troposphere between these two cases cause the different circulations at the surface that impact the evolution of the dust storms differently.
    [Show full text]
  • Community Structure Through Time: `Ubeidiya, a Lower Pleistocene Site As a Case Study
    Community Structure through Time: `Ubeidiya, a Lower Pleistocene Site as a Case Study Thesis submitted for the degree of “Doctor of Philosophy” by Miriam Belmaker Submitted to the Senate of the Hebrew University March 2006 This work was carried out under the supervision of Prof. Eitan Tchernov Prof. Ofer Bar Yosef Prof. Uzi Motro this thesis is dedicated to Eitan Tchernov, my mentor, without whom this thesis would have never happened Contents Acknowledgments xii Abstract xiv I Framework 1 1 Introduction 2 2 The Site of `Ubeidiya 9 2.1 Geology and stratigraphy of the `Ubeidiya Formation . 9 2.2 Dating of the `Ubeidiya Formation . 10 2.3 Excavation history . 15 2.4 Previous paleoecological research . 17 2.5 The presence of early hominins at `Ubeidiya . 19 II Methodology 22 3 Paleontological Methodology 23 3.1 Stratigraphy . 23 3.1.1 Assignment of specimens to stratigraphic units . 23 3.1.2 Choice of strata for analysis . 25 3.2 Taxonomy . 26 3.2.1 Identification of specimens . 26 3.2.2 Choice of taxa for analysis . 28 3.3 Quantification . 30 3.3.1 Quantification of individuals per species . 30 3.3.2 Quantification of body elements . 31 i 4 Identification of Pattern of Persistence or Change in the Large Mammalian Commu- nity throughout the `Ubeidiya Sequence 34 4.1 The statistical model . 34 4.2 Independent variables of the null hypotheses: The taphonomy of the `Ubeidiya large mammal assemblages . 37 4.2.1 Weathering . 37 4.2.2 Fluvial transport . 39 4.2.3 Agents of accumulation . 41 4.2.4 Post depositional carnivore ravaging .
    [Show full text]
  • Rock Art in the Hail Region of Saudi Arabia 
    Rock art in the Hail Region of Saudi Arabia Rock Art in the Hail Region of Saudi Arabia SERIAL NOMINATION OF Jabal Umm Sinman, Jubbah and Jabal al-Manjor / Jabal Raat, Shuwaymis Submitted by the Saudi Commission for Tourism and Antiquities as a proposal for inclusion in the UNESCO World Heritage List as a Serial Nomination 2013 / 2014 AD - 1434 / 1435AH Rock art in the Hail Region of Saudi Arabia 1 Rock Art in the Hail Region of Saudi Arabia SERIAL NOMINATION OF Jabal Umm Sinman, Jubbah and Jabal al-Manjor / Jabal Raat, Shuwaymis Submitted by the Saudi Commission for Tourism and Antiquities as a proposal for inclusion in the UNESCO World Heritage List as a Serial Nomination 2013 / 2014 AD - 1434 / 1435AH Rock Art in the Hail Region of Saudi Arabia Executive Summary State Party Kingdom of Saudi Arabia State, Province Northern Province, Hail Region or Region Name of Rock art in the Hail Region of Saudi Arabia Property Serial Serial nomination of two properties: properties 1. Rock art at Jabal Umm Sinman, Jubbah and 2. Rock art at Jabal al-Manjor and Jabal Raat, Wadi al-Mukhayet, Shuwaymis Geographical 1. Jabal Umm Sinman, Jubbah: coordinates 28° 00’ 33” N, 40° 55’ 44” E to the nearest 2. Jabal al-Manjor and Jabal Raat at Shuwaymis: second 26° 09’ 13” N, 39° 53’ 48” E Textual 1. Jabal Umm Sinman, Jubbah, 90 km northwest of Hail, is bounded in description the west, north and south by desert sands and in the east by a security of the fence that borders the town of Jubbah.
    [Show full text]
  • Abstract Pluvial Deposits in Mudawwara, Jordan And
    ABSTRACT PLUVIAL DEPOSITS IN MUDAWWARA, JORDAN AND THEIR IMPLICATIONS FOR MEDITERRANEAN AND MONSOONAL PRECIPITATION IN THE LEVANT by Gentry Ann Catlett Deposits in the hyper-arid Mudawwara basin of Jordan are examined to understand the timing and source of past pluvial episodes in the southern Levant. Mineralogical, geochemical, and radiocarbon analysis of a 2.35m core from dry playa Khabrat Ratiya suggest sedimentation from ~29-21 ka BP, coinciding with the highest lake levels of Paleolake Lisan. Coquina deposits in Mudawwara have been attributed to paleolake(s) sustained by intensified tropical monsoonal precipitation from 88-170 ka by Petit-Maire et al. (2010, Global and Planetary Change 72: 368-373). However, we argue that closed- system behavior has not been demonstrated for the U-series ages on these shells and geomorphologic evidence suggests an older depositional age. We suggest that in southern Jordan (1) pluvial episodes occurred in Khabrat Ratiya ~29-21 ka and resulted from increased winter precipitation from the Mediterranean, and (2) the Mudawwara coquina deposits should not be used as evidence for tropical monsoonal precipitation during interglacial periods. PLUVIAL DEPOSITS IN MUDAWWARA, JORDAN AND THEIR IMPLICATIONS FOR MEDITERRANEAN AND MONSOONAL PRECIPITATION IN THE LEVANT A Thesis Submitted to the Faculty of Miami University in partial fulfillment of the requirements for the degree of Master of Science Department of Geology and Environmental Earth Science by Gentry Ann Catlett Miami University Oxford, Ohio 2014 Advisor: Jason A. Rech Reader: Ellen Currano Committee Member: Elisabeth Widom TABLE OF CONTENTS 1. Introduction ....................................................................................................................................... 1 2. Regional Setting ............................................................................................................................... 2 2.1 Modern Climate ..................................................................................................................
    [Show full text]
  • Articles Bring Nutrients Longstreth Et Al., 1995; Bennett Et Al., 2006; Bennion Et Al., to Marine Ecosystems, Which Is Especially Important for the 2007)
    Atmos. Chem. Phys., 15, 199–222, 2015 www.atmos-chem-phys.net/15/199/2015/ doi:10.5194/acp-15-199-2015 © Author(s) 2015. CC Attribution 3.0 License. The impact of dust storms on the Arabian Peninsula and the Red Sea P. Jish Prakash, G. Stenchikov, S. Kalenderski, S. Osipov, and H. Bangalath Division of Physical Sciences and Engineering, King Abdullah University of Science and Technology, Thuwal, Saudi Arabia Correspondence to: G. Stenchikov ([email protected]) Received: 24 February 2014 – Published in Atmos. Chem. Phys. Discuss.: 22 July 2014 Revised: 3 November 2014 – Accepted: 26 November 2014 – Published: 12 January 2015 Abstract. Located in the dust belt, the Arabian Peninsula is 1 Introduction a major source of atmospheric dust. Frequent dust outbreaks and some 15 to 20 dust storms per year have profound ef- Mineral dust is the dominant atmospheric aerosol (Buseck fects on all aspects of human activity and natural processes and Posfai, 1999). It plays an important role in the Earth’s in this region. To quantify the effect of severe dust events climate system, although the magnitude and even the sign of on radiation fluxes and regional climate characteristics, we its radiative effect at the top of the atmosphere (TOA) remain simulated the storm that occurred from 18 to 20 March 2012 uncertain. Most airborne dust is generated in desert and semi- using a regional weather research forecast model fully cou- desert areas and transported across local to global scales. pled with the chemistry/aerosol module (WRF–Chem). This Dust storms lift millions of tons of dust into the at- storm swept over a remarkably large area affecting the entire mospheric boundary layer.
    [Show full text]
  • Integrated Geological, Hydrogeological, and Geophysical Investigations of a Barchan Sand Dune in the Eastern Region of Saudi Arabia
    water Article Integrated Geological, Hydrogeological, and Geophysical Investigations of a Barchan Sand Dune in the Eastern Region of Saudi Arabia Mohammed Benaafi 1,*, Sherif M. Hanafy 2, Abdullatif Al-Shuhail 2 , Ammar El-Husseiny 2 and Jack Dvorkin 2 1 Center for Environment and Water, King Fahd University of Petroleum & Minerals, Dhahran 34464, Saudi Arabia 2 College of Petroleum Engineering and Geosciences, King Fahd University of Petroleum & Minerals, Dhahran 34464, Saudi Arabia; [email protected] (S.M.H.); [email protected] (A.A.-S.); [email protected] (A.E.-H.); [email protected] (J.D.) * Correspondence: benaafi@kfupm.edu.sa Received: 15 January 2020; Accepted: 25 February 2020; Published: 2 March 2020 Abstract: In arid countries such as Saudi Arabia, aeolian sand often covers a large area of the country. Understanding the variations of sand properties in dunes, including grain size, sorting, mineral composition and water content, can be important for groundwater recharge, environmental, and construction applications. Earlier studies examined properties of sand dunes by collecting samples from the surface. This study aims to investigate variations of sand properties within a Barchan sand dune in the coastal area of Saudi Arabia, by collecting samples and measurements from two vertically drilled boreholes up to the ground water level; one drilled in the dune crest and another one in the limb. Representative samples were collected and analyzed for their texture parameters, water content, and mineralogy. Electrical resistivity survey data was also acquired to map water content variation in the dune limb, and for comparison with well bore data.
    [Show full text]
  • 1 Trajectory Analysis of Saudi Arabian Dust Storms 1 2 Michael Notaro 3
    1 1 Trajectory Analysis of Saudi Arabian Dust Storms 2 3 Michael Notaro 4 Nelson Center for Climatic Research, University of Wisconsin-Madison 5 1225 West Dayton Street, Madison, Wisconsin 53706 6 * [email protected], 608-261-1503 7 8 Fahad Alkolibi, Eyad Fadda, Fawzieh Bakhrjy 9 King Saud University 10 11 Revised Research Article to the Journal of Geophysical Research-Atmospheres 12 13 Abstract 14 15 Temporal and spatial characteristics of Saudi Arabian dust storms, with focus on 16 associated air parcel trajectories, are investigated using station and gridded weather 17 observations and remotely-sensed aerosol optical depth (AOD). For 13 focal stations, an 18 extensive pool of 84-hour backward trajectories is developed for dust storm days, and the 19 trajectories are grouped into 3-5 representative clusters based on the K-means technique 20 and Silhouette Coefficients. 21 Saudi Arabian dust storms are most prominent during February-June, with a mid- 22 winter peak along the southern coast of the Red Sea, spring peak across northern Saudi 23 Arabia around the An Nafud Desert, and early summer peak in eastern Saudi Arabia around 24 the Ad Dahna Desert. Based on backward trajectories, the primary local dust source is the 25 Rub Al Khali Desert and the primary remote sources are the Saharan Desert, for western 26 Saudi Arabia, and Iraqi Deserts, for northern and eastern Saudi Arabia. During February- 27 April, the Mediterranean storm track is active, with passing cyclones and associated cold 28 fronts carrying Saharan dust to Saudi Arabian stations along the northern coast of the Red 29 Sea.
    [Show full text]