Sunshine Duration As a Proxy of the Atmospheric Aerosol Content

Total Page:16

File Type:pdf, Size:1020Kb

Sunshine Duration As a Proxy of the Atmospheric Aerosol Content SUNSHINE DURATION AS A PROXY OF THE ATMOSPHERIC AEROSOL CONTENT Alejandro Sanchez Romero Per citar o enllaçar aquest document: Para citar o enlazar este documento: Use this url to cite or link to this publication: http://hdl.handle.net/10803/394045 ADVERTIMENT. L'accés als continguts d'aquesta tesi doctoral i la seva utilització ha de respectar els drets de la persona autora. Pot ser utilitzada per a consulta o estudi personal, així com en activitats o materials d'investigació i docència en els termes establerts a l'art. 32 del Text Refós de la Llei de Propietat Intel·lectual (RDL 1/1996). Per altres utilitzacions es requereix l'autorització prèvia i expressa de la persona autora. En qualsevol cas, en la utilització dels seus continguts caldrà indicar de forma clara el nom i cognoms de la persona autora i el títol de la tesi doctoral. No s'autoritza la seva reproducció o altres formes d'explotació efectuades amb finalitats de lucre ni la seva comunicació pública des d'un lloc aliè al servei TDX. Tampoc s'autoritza la presentació del seu contingut en una finestra o marc aliè a TDX (framing). Aquesta reserva de drets afecta tant als continguts de la tesi com als seus resums i índexs. ADVERTENCIA. El acceso a los contenidos de esta tesis doctoral y su utilización debe respetar los derechos de la persona autora. Puede ser utilizada para consulta o estudio personal, así como en actividades o materiales de investigación y docencia en los términos establecidos en el art. 32 del Texto Refundido de la Ley de Propiedad Intelectual (RDL 1/1996). Para otros usos se requiere la autorización previa y expresa de la persona autora. En cualquier caso, en la utilización de sus contenidos se deberá indicar de forma clara el nombre y apellidos de la persona autora y el título de la tesis doctoral. No se autoriza su reproducción u otras formas de explotación efectuadas con fines lucrativos ni su comunicación pública desde un sitio ajeno al servicio TDR. Tampoco se autoriza la presentación de su contenido en una ventana o marco ajeno a TDR (framing). Esta reserva de derechos afecta tanto al contenido de la tesis como a sus resúmenes e índices. WARNING. Access to the contents of this doctoral thesis and its use must respect the rights of the author. It can be used for reference or private study, as well as research and learning activities or materials in the terms established by the 32nd article of the Spanish Consolidated Copyright Act (RDL 1/1996). Express and previous authorization of the author is required for any other uses. In any case, when using its content, full name of the author and title of the thesis must be clearly indicated. Reproduction or other forms of for profit use or public communication from outside TDX service is not allowed. Presentation of its content in a window or frame external to TDX (framing) is not authorized either. These rights affect both the content of the thesis and its abstracts and indexes. DOCTORAL THESIS SUNSHINE DURATION AS A PROXY OF THE ATMOSPHERIC AEROSOL CONTENT Alejandro Sanchez Romero 2016 DOCTORAL THESIS SUNSHINE DURATION AS A PROXY OF THE ATMOSPHERIC AEROSOL CONTENT Alejandro Sanchez Romero 2016 Doctoral Programme in Experimental Sciences and Sustainability Supervisors: Josep Calbó Angrill José Abel González Gutiérrez Presented in partial fulfilment of the requirements for a doctoral degree from the University of Girona Dr. Josep Calbó Angrill and Dr. José Abel González Gutiérrez, of Department of Physics Universitat de Girona, WE DECLARE: That the thesis entitled ―Sunshine duration as a proxy of the atmospheric aerosol content‖, presented by Alejandro Sanchez Romero to obtain a doctoral degree, has been completed under our supervision and meets the requirements to opt for an International Doctorate. For all intents and purposes, we hereby sign this document. Dr. Josep Calbó Angrill Dr. José Abel González Gutiérrez Girona, May 2nd, 2016. List of publications This Ph.D. thesis includes one review paper and three research papers that have been published in peer-reviewed journals. The complete references of the papers comprised in this thesis and the corresponding impact factor of the journals, according to the 2014 Journal Citation Reports (JCR), are: 1. Sanchez-Romero, A., Sanchez-Lorenzo, A., Calbó, J., González, J.A., and Azorin- Molina, C. (2014), The signal of aerosol-induced changes in sunshine duration records: A review of the evidence, Journal of Geophysical Research Atmosphere, 119, 4657–4673, doi:10.1002/2013JD021393. (Impact factor: 3.426; position 19/175; Category: Geosciences, Multidisciplinary; 1st quartile). 2. Sanchez-Romero, A., González, J. A., Calbó, J., and Sanchez-Lorenzo, A. (2015), Using digital image processing to characterize the Campbell–Stokes sunshine recorder and to derive high-temporal resolution direct solar irradiance, Atmospheric Measurement Techniques, 8, 183-194, doi:10.5194/amt-8-183-2015. (Impact factor: 2.929; position 20/77; Category: Meteorology & Atmospheric Sciences; 2nd quartile). 3. Sanchez-Romero, A., González, J. A., Calbó, J., and Sanchez-Lorenzo, A., and Michalsky, J. (2016), Aerosol optical depth in a western Mediterranean site: an assessment of different methods, Atmospheric Research, 174-175, 70-84, doi:10.1016/j.atmosres.2016.02.002. (Impact factor: 2.844; position 22/77; Category: Meteorology & Atmospheric Sciences; 2nd quartile) 4. Sanchez-Romero, A., Sanchez-Lorenzo, A., González, J.A., and Calbó, J. (2016), Reconstruction of long-term aerosol optical depth series with sunshine duration records, Geophysical Research Letters, 43, 1296–1305, doi:10.1002/2015GL067543. (Impact factor: 4.196; position 9/175; Category: Geosciences Multidisciplinary; 1st quartile) Two other articles related with the subject of the thesis have also been co-authored by the author of this thesis, but are not included in it: 1. Sanchez-Lorenzo, A., Calbó, J., Wild, M., Azorin-Molina, C., and Sanchez-Romero, A. (2013), New insights into the history of the Campbell-Stokes sunshine recorder. Weather, 68: 327-331, doi: 10.1002/wera.2130. 2. Sanchez-Lorenzo, A., Enriquez-Alonso, A., Wild, M., Trentmann, J., Vicente-Serrano, S.M., Sanchez-Romero, A., Posselt, R., and Hakuba, M. (2016), Trends in downward surface solar radiation from satellites and ground observations over Europe during 1983- 2010, Remote Sensing of Environment (in progress). There is nothing so stable as change Bob Dylan Acknowledgments Com en una marató, aquest ha estat un llarg camí per recórrer. Aquesta tesi posa punt i final a una de les etapes més maques de la meva vida. Tancar etapes sempre genera certa tristesa, però sé que després vindran nous reptes i això sempre es motivador. M’he pres la llibertat d’escriure aquesta secció en la meva llengua, per tal de poder expressar la més sincera gratitud a un nombre de persones (tot i que no dubto que algú em deixaré), sense les quals aquesta tesi mai hagués estat completada. En primer lloc, m’agradaria agrair als meus directors de tesi, en Josep Calbó i en Josep-Abel González (o com són més coneguts en el departament, els Joseps), per la seva dedicació i suport durant aquests anys. Així mateix, per haver-me transmès el rigor, esperit científic i honestedat intel·lectual necessaris per moure’m en un món, el de la investigació científica, cada vegada més competitiu. Arturo, la burocràcia, les normatives i els papers no entenen ni reflecteixen les relacions humanes, però està clar que la confiança, el suport i el coneixement que m’has aportat des del primer dia reflectirien, i de sobres, el teu paper com a codirector d’aquesta tesi. A més, ningú m’ha aportat tantes hores de lectura com els teus correus. Agrair també en César que ha aconseguit encomanar-me la seva passió per un instrument tan simple i rudimentari com és l’heliògraf Campbell-Stokes. A continuació, vull donar les gràcies a totes les companyes i companys del grup i de despatx en general: Aaron, Victor, Montse, Ios, Conxi, Alex, Bruna, Dani, etc. Sou genials! Gràcies per tot el que hem compartit, pels milers de cafès, per totes les hores de pensar, llegir, d’escriure….No voldria oblidar-me del Servei Personal Administratiu del Departament de Física, sobretot de l’Anna Espígol, en Xevi Baca, i en Xicu Gómez, que han fet que els problemes administratius i tècnics (que no han estat pocs) hagin estat pura anècdota. Agrair també a Joseph Michalsky i John Augustine, que van fer de la meva estada a Estats Units una gran experiència. Sobre el paper, investigadors de renom mundial amb molta experiència en el món de la recerca. En la realitat, això i més, persones properes, directes, honestes i que mai tenen un no per resposta. Moltes gràcies per la vostra ajuda. No m’oblido tampoc dels meus companys en la casa de la sra. Lorna Pollard (la nostra petita representació de la ONU), poques coses hi ha més gratificants que les xerrades multiculturals que vam compartir. He de recordar a tots aquells amics amb qui he compartit trajecte vital durant aquests anys, molt especialment, Robert, Tates, Carlos, Ali, Puxi, Tresa, David, Sònia, Javi, Estefania, Adri, Nàndez, Sarita, així com molts altres, espero que es donin per al·ludits. A tots aquells que alguna vegada em van dedicar 5 minuts del seu temps perquè els expliqués què dimonis estava investigant, sincerament, gràcies! Finalment i no per això menys important, no hi ha paraules de agraïment als meus pares, per la vostra estima incondicional, per la immensa llibertat que m’heu donat i per respectar sempre les meves decisions. També vull donar les gràcies a la meva germana, la Silvia, qui sempre m’ha animat a superar-me a mi mateix, tot i el meu passotisme i la distància que ens separa.
Recommended publications
  • Watching the Weather Since 1885: the History and Climate Record of the Blue Hill Meteorological Observatory
    Watching the Weather Since 1885: The History and Climate Record of the Blue Hill Meteorological Observatory Michael J. Iacono Atmospheric and Environmental Research, Blue Hill Meteorological Observatory Massachusetts Watchmakers and Clockmakers Association 19 November 2019 Outline • Long View of Climate Change • Observatory History • Traditional Instruments • Blue Hill Climate bluehill.org/observatory BHO Mission: ”To foster public understanding of and appreciation for atmospheric science, while continuing to maintain a meticulous record of weather observations for the long-term study of climate.” Climate Change: What’s the Big Picture? • 5-10 degrees F colder during last Ice Age (20,000 yrs ago) • 10-20 degrees F warmer during Jurassic Period (65 Mya) • Stable climate for the last 10,000 years very unusual Climate Change: What’s the Big Picture? • Large climate changes have occurred regularly in Earth’s history due to natural factors: • Orbital variations (change incoming solar energy) • Volcanic eruptions (vent greenhouse gases: CO2) • Asteroid impacts (eject material that obscures sun) • Continental drift (alters air and ocean circulation) • Currently in inter-glacial period with some ice cover • Human Factor: Fossil fuel use has increased carbon dioxide to highest level in 3 million years (up from 280 to 415 ppm in 150 years) Climate Change: Role of Orbital Variations • Changes in Earth’s movement affect climate • Can think of Earth and Sun as precise time pieces • Earth’s Axis Tilt (23.5 degrees; affects change of seasons) • Controls
    [Show full text]
  • Simple Weather Measurements at School Or at Home
    SIMPLE WEATHER MEASUREMENTS AT SCHOOL OR AT HOME Geoff Jenkins 6th Edition ROYAL METEOROLOGICAL SOCIETY 104 OXFORD ROAD READING BERKSHIRE RG1 7LL Telephone: +44 (0)118 956 8500 Fax: +44 (0)118 956 8571 E-mail: [email protected] WWW: http://www.royalmetsoc.org/ Registered Charity Number 208222 Copyright © 1999 Royal Meteorological Society Reprinted November 2000 ISBN 0 948 090 13 8 SIMPLE WEATHER MEASUREMENTS AT SCHOOL OR AT HOME INTRODUCTION Making observations is an essential part of learning about the weather. This has been recognised by many teachers for years and is now enshrined in British National Curricula. In Geography Programmes of Study, for example, children aged 7 to 11 are required to undertake fieldwork and to carry out investigations that involve the use of instruments to make measurements. In the experimental and investigative parts of Science Programmes of Study, too, weather measurements help provide insight into concepts being taught. This booklet looks at ways in which simple weather measurements can be made with a minimum of cost or fuss. It has been written primarily as guidance for schoolteachers, particularly those in junior and middle schools. Hence, there are many references to educational aspects and considerations. However, many of the ideas will also be of interest to amateurs thinking of setting up a weather station at home. Suggestions are given as to suitable instruments and methods for taking crude but effective weather records, when it does not really matter if the temperature is a degree or two in error, or the rain-gauge does not have the ideal exposure to catch all the rain properly.
    [Show full text]
  • Study on Local Cloud Coverage Using Ground-Based Measurement of Solar Radiation
    Study on Local Cloud Coverage Using Ground-Based Measurement of Solar Radiation Sweata Sijapati Study on Local Cloud Coverage Using Ground-Based Measurement of Solar Radiation Dissertation Submitted to the Faculty of Civil and Environmental Engineering In Partial Fulfillment of the Requirements for the Degree of Doctor at Ehime University By Sweata Sijapati June 2016 Advisor: Professor Ryo Moriwaki Dedicated to my parents It’s your support and motivation that has made me stronger CERTIFICATION This is to certify that the dissertation entitled, “Study on Local Cloud Coverage Using Ground-Based Measurement of Solar Radiation” presented by Ms. Sijapati Sweata in partial fulfillment of the academic requirement of the degree of doctor has been examined and accepted by the evaluation committee at Graduate School of Science and Engineering of Ehime University. …………………………………. Ryo Moriwaki Professor of Civil and Environmental Engineering Thesis Advisor / Examiner 1 …………………………………. ……………. of Civil and Environmental Engineering Examiner 2 …………………………………. ……………. of Civil and Environmental Engineering Examiner 3 TABLE OF CONTENTS LIST OF FIGURES ........................................................................................................... IX LIST OF TABLES ............................................................................................................ XV LIST OF ABBREVIATION .......................................................................................... XVI LIST OF SYMBOL ....................................................................................................
    [Show full text]
  • Development of a Model for Prediction of Solar Radiation
    ENGINEERENGINEER - - Vol. Vol. XLVIII, XLVIII No., No. 03, 03 pp., pp. [19-25], [page 2015range], 2015 ©© TheThe Institution Institution of of Engineers, Engineers, Sri SriLanka Lanka Development of a Model for Prediction of Solar Radiation W. D. A. S. Wijayapala and D. H. K. Kushal Abstract: Power generation from renewable energy sources such as wind, mini-hydro, solar etc is becoming increasingly popular due to environmental concerns. However, it is not possible to predict the energy generation of solar power plants in advance. Hence the power system operator has no information about the tomorrow‟s possible energy availability from these non-dispatchable power plants. The outcome of this study enables the system operator to predict the possible energy generation from solar power plants based on the weather forecasts and provide the system operator with predictions on energy generation and capacity of solar power plants connected to the grid. The predictions will enable to prepare the dispatch schedules accordingly. In this study, the effect of the geographical and meteorological parameters for predicting daily global solar radiation at Sooriyawewa, Hambantota in Sri Lanka is investigated. A multiple linear regression was applied to explain the relationship among solar radiation and identified meteorological and geographical parameters such as cloud cover, sunshine duration, precipitation, open air temperature, relative humidity, wind speed, gust speed and sine value of declination angle. Variables in these equations were used to estimate the global solar radiation. Values calculated/predicted from models were compared with the actual measurements to validate the model. Keywords : Solar Power, Solar Radiation, Prediction The most important usage of this model is that 1.
    [Show full text]
  • Proceedings of the Inter-Regional Workshop March 22-26, 2004, Manila, Philippines
    Strengthening Operational Agrometeorological Services at the National Level Proceedings of the Inter-Regional Workshop March 22-26, 2004, Manila, Philippines Strengthening Operational Agrometeorological Services at the National Level ______________________________________________________ Proceedings of the Inter-Regional Workshop March 22-26, 2004, Manila, Philippines Editors Raymond P. Motha M.V.K. Sivakumar Michele Bernardi Sponsors United States Department of Agriculture Office of the Chief Economist World Agricultural Outlook Board Washington, D.C. 20250, USA World Meteorological Organization Agricultural Meteorology Division 7bis, Avenue de la Paix 1211 Geneva 2, Switzerland Food and Agriculture Organization of the United Nations Environment and Natural Resources Service Viale delle Terme di Caracalla 00100 Rome, Italy Philippine Atmospheric Geophysical and Astronomical Services Administration Science Garden Complex Agham Road, Dilliman, Quezon City Philippines 1100 Series WAOB-2006-1 AGM-9 WMO/TD NO. 1277 Washington, D.C. 20250 January 2006 Proper citation is requested. Citation: Raymond P. Motha, M.V.K. Sivakumar, and Michele Bernardi (Eds.) 2006. Strengthening Operational Agrometeorological Services at the National Level. Proceedings of the Inter-Regional Workshop, March 22-26, 2004, Manila, Philippines. Washington, D.C., USA: United States Department of Agriculture; Geneva, Switzerland: World Meteorological Organization; Rome, Italy: Food and Agriculture Organization of the United Nations. Technical Bulletin WAOB-2006-1 and AGM-9,
    [Show full text]
  • Impact of Urbanization on Sunshine Duration from 1987 to 2016 in Hangzhou City, China
    atmosphere Article Impact of Urbanization on Sunshine Duration from 1987 to 2016 in Hangzhou City, China Kai Jin 1,2,* , Peng Qin 1 , Chunxia Liu 1, Quanli Zong 1 and Shaoxia Wang 1,* 1 Qingdao Engineering Research Center for Rural Environment, College of Resources and Environment, Qingdao Agricultural University, Qingdao 266109, China; [email protected] (P.Q.); [email protected] (C.L.); [email protected] (Q.Z.) 2 State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Water and Soil Conservation, Northwest A&F University, Yangling 712100, China * Correspondence: [email protected] (K.J.); [email protected] (S.W.); Tel.: +86-150-6682-4968 (K.J.); +86-136-1642-9118 (S.W.) Abstract: Worldwide solar dimming from the 1960s to the 1980s has been widely recognized, but the occurrence of solar brightening since the late 1980s is still under debate—particularly in China. This study aims to properly examine the biases of urbanization in the observed sunshine duration series from 1987 to 2016 and explore the related driving factors based on five meteorological stations around Hangzhou City, China. The results inferred a weak and insignificant decreasing trend in annual mean sunshine duration (−0.09 h/d decade−1) from 1987 to 2016 in the Hangzhou region, indicating a solar dimming tendency. However, large differences in sunshine duration changes between rural, suburban, and urban stations were observed on the annual, seasonal, and monthly scales, which can be attributed to the varied urbanization effects. Using rural stations as a baseline, we found evident urbanization effects on the annual mean sunshine duration series at urban and suburban stations—particularly in the period of 2002–2016.
    [Show full text]
  • Variation in Surface Air Temperature of China During the 20Th Century
    Journal of Atmospheric and Solar-Terrestrial Physics 73 (2011) 2331–2344 Contents lists available at ScienceDirect Journal of Atmospheric and Solar-Terrestrial Physics journal homepage: www.elsevier.com/locate/jastp Variation in surface air temperature of China during the 20th century Willie Soon a,n, Koushik Dutta b, David R. Legates c, Victor Velasco d, WeiJia Zhang e a Harvard-Smithsonian Center for Astrophysics, Cambridge, MA 02138, USA b Large Lakes Observatory, University of Minnesota-Duluth, Duluth, MN 55812, USA c College of Earth, Ocean, and Environment, University of Delaware, Newark, DE 19716, USA d Departamento de Investigaciones Solares y Planetarias, Instituto de Geofisica, Universidad Nacional Autonoma de Mexico, Ciudad Universitaria, C.P. 04510, Mexico e Department of Physics, Peking University, Beijing 100871, China article info abstract Article history: The 20th century surface air temperature (SAT) records of China from various sources are analyzed Received 21 March 2011 using data which include the recently released Twentieth Century Reanalysis Project dataset. Two key Received in revised form features of the Chinese records are confirmed: (1) significant 1920s and 1940s warming in the 20 July 2011 temperature records, and (2) evidence for a persistent multidecadal modulation of the Chinese surface Accepted 25 July 2011 temperature records in co-variations with both incoming solar radiation at the top of the atmosphere as Available online 3 August 2011 well as the modulated solar radiation reaching ground surface. New evidence is presented for this Keywords: Sun–climate link for the instrumental record from 1880 to 2002. Additionally, two non-local physical Total solar irradiance aspects of solar radiation-induced modulation of the Chinese SAT record are documented and Sunshine duration discussed.
    [Show full text]
  • Climate Change and Global Warming, Introduction to Various Meteorological Equipments Subject: AGRICULTURE
    Class Notes Class: XI Topic: Climate change and global warming, Introduction to various meteorological equipments Subject: AGRICULTURE UNIT-II Climate change and global warming Climate change, also called global warming, refers to the rise in average surface temperatures on Earth. Temperature records going back to the late 19th Century show that the average temperature of the Earth's surface has increased by about 0.8C (1.4F) in the last 100 years. About 0.6C (1.0F) of this warming occurred in the last three decades. Satellite data shows an average increase in global sea levels of some 3mm per year in recent decades. The Greenland Ice Sheet has experienced record melting in recent years; if the entire 2.8 million cubic km sheet were to melt, it would raise sea levels by 6m. Satellite data shows the West Antarctic Ice Sheet is also losing mass, and a recent study indicated that East Antarctica, which had displayed no clear warming or cooling trend, may also have started to lose mass in the last few years. But scientists are not expecting dramatic changes. In some places, mass may actually increase as warming temperatures drive the production of more snows. The effects of a changing climate can also be seen in vegetation and land animals. These include earlier flowering and fruiting times for plants and changes in the territories (or ranges) occupied by animals. Causes of Global Warming Greenhouse Gases Some gases in the Earth's atmosphere act a bit like the glass in a greenhouse, trapping the sun's heat and stopping it from leaking back into space.
    [Show full text]
  • The Scottish Coastal Observatory 1997-2013 Part 2
    The Scottish Coastal Observatory 1997-2013 Part 2 - Description of Scotland’s Coastal Waters Scottish Marine and Freshwater Science Vol 7 No 26 E Bresnan, K Cook, J Hindson, S Hughes, J-P Lacaze, P Walsham, L Webster and W R Turrell The Scottish Coastal Observatory 1997-2013 Part 2 – Description of Scotland’s coastal waters Scottish Marine and Freshwater Science Vol 7 No 26 E Bresnan, K Cook, J Hindson, S Hughes, J-P Lacaze, P Walsham, L Webster and W R Turrell Published by Marine Scotland Science ISSN: 2043-772 DOI: 10.7489/1881-1 Marine Scotland is the directorate of the Scottish Government responsible for the integrated management of Scotland’s seas. Marine Scotland Science (formerly Fisheries Research Services) provides expert scientific and technical advice on marine and fisheries issues. Scottish Marine and Freshwater Science is a series of reports that publishes results of research and monitoring carried out by Marine Scotland Science. It also publishes the results of marine and freshwater scientific work carried out by Marine Scotland under external commission. These reports are not subject to formal external peer-review. This report presents the results of marine and freshwater scientific work carried out by Marine Scotland Science. © Crown copyright 2016 You may re-use this information (excluding logos and images) free of charge in any format or medium, under the terms of the Open Government Licence. To view this licence, visit: http://www.nationalarchives.gov.uk/doc/open- governmentlicence/version/3/ or email: [email protected]. Where we have identified any third party copyright information you will need to obtain permission from the copyright holders concerned.
    [Show full text]
  • Forecasting of Severe Thunderstorms Using Upper Air Data
    International Journal of Scientific & Engineering Research, Volume 6, Issue 7, July-2015 306 ISSN 2229-5518 Forecasting of Severe Thunderstorms using Upper Air data Sonia Bhattacharya, Anustup Chakrabarty and Himadri Chakrabarty Abstract— Severe local thunderstorm is the extreme weather convective phenomenon generated from cumulonimbus cloud. It has a devastating effect on human life. Correct forecasting is very crucial factor to save life and property. Here in this paper we have applied artificial neural network to achieve desired result. Multilayer perceptron has been applied on upper air data such as sunshine hour, pressure at freezing level, height at freezing level and cloud coverage (octa NH). MLP predicted correctly both ‘squall’ and ‘no squall’ storm days more than 90% with 12 hours leading time. Index Terms— MLP, squall, cumulus cloud, sunshine hour, pressure at freezing level, height at freezing level, octa 1 INTRODUCTION University Kolkata, India, PH-919433355720, E-mail: [email protected] When not obscured by haze or other clouds, the Thunderstorm is one of the most devastating top of a cumulonimbus is bright and tall, reaching up to an altitude of 10-16 km (lower in higher type of mesoscale, convective weather latitudes and higher in the tropics). Although a phenomenon, generated from the cumulonimbus thunderstorm is a three-dimensional structure, it cloud. It occurs in different subtropical places of should be thought of as a constantly evolving the world, (Ludlam, 1963). Over 40,000 process rather than an object. Each thunderstorm, thunderstorms occur throughout the world each or cluster of thunderstorms, is a self-contained day[1] The strong wind which has the speed of at system with organized regions of up drafts least 45 kilometers per hour with the duration of (upward moving air) and downdrafts (downward minimum 1 secondIJSER is termed as squall [1].
    [Show full text]
  • A Guide for Amateur Observers to the Exposure and Calibration Of
    A Guide to the Siting, Exposure and Calibration of Automatic Weather Stations for Synoptic and Climatological Observations By Andrew K. Overton © Andrew K. Overton 2009 1 Contents Introduction......................................................................................................................................... 3 Siting and Exposure.................................................. ......................................................................... 3-7 Temperature and relative humidity......................................................................................... 4, 5 Precipitation............................................................................................................................ 5, 6 Wind speed and direction........................................................................................................ 6, 7 Sunshine, solar & UV radiation............................................................................................... 7 Calibration........................................................................................................................................... 7-15 Pressure................................................................................................................................... 9 Air temperature....................................................................................................................... 10 Grass minimum and soil temperature....................................................................................
    [Show full text]
  • 2018 Climate Summary
    & ~ Hurricane Season Review ~ Meteorological Department St. Maarten Modesta Drive # 12, Simpson Bay (721) 545-4226 www.meteosxm.com MDS Climatological Summary 2018 The information contained in this Climatological Summary must not be copied in part or any form, or communicated for the use of any other party without the expressed written permission of the Meteorological Department St. Maarten. All data and observations were recorded at the Princess Juliana International Airport. This document is published by the Meteorological Department St. Maarten, and a digital copy is available on our website. Prepared by: Sheryl Etienne-Leblanc Published by: Meteorological Department St. Maarten Modesta Drive # 12, Simpson Bay St. Maarten, Dutch Caribbean Telephone: (721) 545-4226 Website: www.meteosxm.com E-mail: [email protected] www.facebook.com/sxmweather www.twitter.com/@sxmweather MDS © May 2019 Page 2 of 29 MDS Climatological Summary 2018 Table of Contents Introduction.............................................................................................................. 4 Island Climatology……............................................................................................. 5 About Us……………………………………………………………………………..……….……………… 6 2018 Hurricane Season Summary…………………………………………………………………………………………….. 8 Local Effects...................................................................................................... 9 Summary Table ...............................................................................................
    [Show full text]