Climate of Turkey
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Journal of International Environmental Application & Science
Journal of International Environmental Application & Science ISSN-1307-0428 Editor in Chief: Prof. Dr. Sukru DURSUN, Environmental Engineering Department, Engineering & Natural Science Faculty, Konya Technical University, Konya, TURKEY EDITORIAL BOARD Prof. Dr. Lynne BODDY Prof. Dr. IR. Raf DEWIL Cardiff School of Biosciences, Main Building, Museum Chemical Eng. Dept, Chemical & Biochem. Process Techn. & Avenue, Cardiff CF10 3TL UK Control Section, Katholieke Un. Leuven, Heverlee, BELGIUM Prof. Dr. Phil INESON Prof. Dr. Tay Joo HWA Stockholm Environment Institute, University of York, Environ. & Water Resources Engineering Division, of Civil & Heslington, York, YO10 5DD, UK Environ. Eng. School, Nanyang Techno. Un., SINGAPORE Prof. Dr. Lidia CRISTEA Dr. Somjai KARNCHANAWONG Romanian Sci. & Arts University, B-dul Energeticienilor, No.9- Environ. Engineering Dept, Faculty of Engineering Chiang Mai 11, Sec. 3, ZC 030796, Bucharest, ROMANIA University, THAILAND Prof. Dr. N. MODIRSHAHLA, Prof. Dr Hab. Boguslaw BUSZEWSK Department of Applied Chemistry, Islamic Azad University, Chemistry & Bioanalytics Environ., Chemistry Faculty, Tabriz Branch, IRAN Nicolaus Copernicus University, Torun, POLAND Prof. Dr. Victor A.DRYBAN, Prof. Dr. Azita Ahmadi-SÉNICHAULT Rock Pressure National Academy of Sciences of Ukraine, Arts et Métiers Paris Tech - Centre de Bordeaux, Esplanade Donetsk, UKRAINE des Arts et Metiers, FRANCE Prof.Dr. Rüdiger ANLAUF Osnabrueck University of Applied Sciences, Osnabrück, Prof. Dr. Irena BARANOWSKA GERMANY Analytical Chemistry Dept., Silesian Technical University, Gliwice, POLAND Prof. Dr. Amjad SHRAIM Chemistry & Earth Sciences Department, College of Arts & Prof. Dr. Indumathi M NAMBI Sciences, Qatar University, Doha, QATAR Indian Institute of Technology Madras, Civil Eng. Dept., Environ. & Water Resources Eng. Div., INDIA Prof. Dr. Massimo ZUCCHETTI Dipartimento di Energetica, Politecnico di Torino, Corso Duca Prof. -
A. FALCONE, V. IACOMI – Archeologia Dell'acqua a Elaiussa
BOLLETTINO DI ARCHEOLOGIA ON LINE DIREZIONE GENERALE ARCHEOLOGIA, BELLE ARTI E PAESAGGIO XI, 2018/1 ANNALISA FALCONE*, VERONICA IACOMI* ARCHEOLOGIA DELL’ACQUA AD ELAIUSSA SEBASTE, CILICIA (TURCHIA): UN CONTESTO DI SCAVO DI ETA’ PROTOBIZANTINA NEL QUARTIERE RESIDENZIALE PRESSO IL PORTO SUD Elaiussa Sebaste (modern Ayaş, Akdeniz Bölgesı, southern Turkey) has been investigated since 1995 by the Italian Archaeological Mission of “Sapienza” University of Rome. Excavations brought to light large sectors of the Roman– Byzantine public area (theatre, agora, baths), necropoleis, two city harbours, the so called “Byzantine palace” and part of the domestic and handcraft quarters. The site was, during the Roman age, one of the most important cities of Cilicia Aspera and maintained its prestigious role as a significant trading port until the late empire and the early Byzantine age, when it became one of the most active centres of LR1 amphoras production. This contri- bution will focus on the “Cura Aquarum Project”, started in 2009 and aimed at identifying, positioning and doc- umenting all the structures related with the water supply of the site. Recognition works were carried out identifying large sections of the aqueduct’s truck, the connected water tanks and numerous cisterns disseminated across the city. Together with the surveys, the complete excavation of one of the cisterns entirely cut in the rock found in the domestic early-Byzantine quarter – luckily sealed just after the site abandonment – contributed to clarify the im- portance of the rainwater harvesting system, even after the aqueduct’s construction, providing a significant portrayal of the latest phase of Elaiussa’s occupation. -
Shankar Ias Academy Test 18 - Geography - Full Test - Answer Key
SHANKAR IAS ACADEMY TEST 18 - GEOGRAPHY - FULL TEST - ANSWER KEY 1. Ans (a) Explanation: Soil found in Tropical deciduous forest rich in nutrients. 2. Ans (b) Explanation: Sea breeze is caused due to the heating of land and it occurs in the day time 3. Ans (c) Explanation: • Days are hot, and during the hot season, noon temperatures of over 100°F. are quite frequent. When night falls the clear sky which promotes intense heating during the day also causes rapid radiation in the night. Temperatures drop to well below 50°F. and night frosts are not uncommon at this time of the year. This extreme diurnal range of temperature is another characteristic feature of the Sudan type of climate. • The savanna, particularly in Africa, is the home of wild animals. It is known as the ‘big game country. • The leaf and grass-eating animals include the zebra, antelope, giraffe, deer, gazelle, elephant and okapi. • Many are well camouflaged species and their presence amongst the tall greenish-brown grass cannot be easily detected. The giraffe with such a long neck can locate its enemies a great distance away, while the elephant is so huge and strong that few animals will venture to come near it. It is well equipped will tusks and trunk for defence. • The carnivorous animals like the lion, tiger, leopard, hyaena, panther, jaguar, jackal, lynx and puma have powerful jaws and teeth for attacking other animals. 4. Ans (b) Explanation: Rivers of Tamilnadu • The Thamirabarani River (Porunai) is a perennial river that originates from the famous Agastyarkoodam peak of Pothigai hills of the Western Ghats, above Papanasam in the Ambasamudram taluk. -
Middle East Meteorology - H.M
TROPICAL METEOROLOGY- Middle East Meteorology - H.M. Hasanean MIDDLE EAST METEOROLOGY H.M. Hasanean Meteorology Department, Faculty of Meteorology, Environment and Arid Land Agriculture, King Abdulaziz University Keywords: Middle East Meteorology, Arid and sub arid climate, Dust storm, Climate change, Circulation systems. Contents 1. Introduction 1.1 Middle East Definition 1.2 Overview of the Middle East Climate 2. Regional climate in the Middle East climate 2.1 Climate of Egypt 2.2 Climate of the Arabian Peninsula an Overview 2.3 Climate of Syria 2.4 Climate of Lebanon 2.5 Climate Jordan 2.6 Climate of Israel and Palestine 2.7 Climate of Cyprus 2.8 Climate of Iraq 2.9 Climate of Turkey 2.10 Climate of Iran 3. Dust storms over the Middle East 3.1 Types of Dust Storms 3.2 Synoptic Analysis of Dust Storms in the Middle East 4. Climate change over the Middle East climate 5. Climate change impacts on water resources in Middle East 6. Circulation systems affect the climate of the Middle East 6.1 Impact of the North Atlantic Oscillation (NAO) on Middle Eastern Climate 6.2 Impact of the El Nino Southern Oscillation (ENSO) on Middle East Climate 6.3 The Role of Highs Pressure (Siberian and Subtropical High Pressure) and Indian Low Pressure on Middle Eastern Climate 6.4 The roleUNESCO of Jet streams on Middle East – Climate EOLSS 7. Conclusion Acknowledgements Glossary SAMPLE CHAPTERS Bibliography Biographical Sketch Summary The Middle East is a region that spans southwestern Asia, western Asia, and northeastern Africa. Although much of the Middle East region has a Mediterranean climate type, i.e. -
Exports: the Heart of Nep
How to Export to 2018 Turkey This report includes all the information related to trade basics and detailed data regarding export from Brazil to Turkey. This report is for information purposes only and Tumer Eng. will not be liable to any direct, indirect, incidental, special, consequential or exemplary damages, including but not limited to, damages for loss of profits, goodwill, use, data, or other intangible losses. Ver:1.0 2018 1 Contents 1 Why Turkey.................................................................................................................................... 12 1.1 General Information .............................................................................................................. 12 1.2 Geography ............................................................................................................................. 13 1.2.1 Distances ....................................................................................................................... 18 1.2.2 Climate of Turkey .......................................................................................................... 19 1.2.2.1 Air temperature changes until now .......................................................................... 20 1.2.2.2 Precipitation changes until now ................................................................................ 21 1.2.2.3 Air temperature changes in the 21st century ........................................................... 21 1.2.2.4 Precipitation changes in the 21st century ................................................................ -
Info for Ankara Applicants
Information for Applicants and Reassignments to the Department of Defense Education Activity’s Ankara Elementary/High School in Ankara, Turkey Ankara Turkey is an UNACCOMPANIED DUTY LOCATION Is Ankara a good fit for you? When deciding, please consider that only the DoDEA employee is authorized to be in Turkey as part of this assignment, you are NOT permitted to have your dependents (family members) with you. This location offers an annual Renewal Agreement for Transportation, allowing employees the opportunity to travel back to the United States (US) to visit family. About Ankara, Turkey Ankara is the capital of Turkey, located in the central part of Anatolia with a population of about 4.5 million, it is Turkey's second-largest city after Istanbul. Ankara has a stable government and economy, it is on this strength, its NATO alliance, and its fairly well-developed infrastructure, it has become a leader in the region. Turkish is the official language; though English is widely understood and is used by some businesses. Islam is the predominant religion of Turkey although places of worship for other faiths exist in the city. Ankara has a continental climate with cold, snowy winters due to its inland location and elevation, and hot, dry summers. Monthly mean temperatures range from 0⁰C (32⁰F) in January to 23⁰C (74⁰F) in July. Ankara E/HS School Community Ankara school opened its doors in 1950 with a staff of 8 servicing a student body of 150 Kindergarten through 9th grade servicing children of US military families. In 1964, the present school buildings, located on a Turkish Military base in Ankara, were dedicated to former U.S. -
Climate Classification Revisited: from Köppen to Trewartha
Vol. 59: 1–13, 2014 CLIMATE RESEARCH Published February 4 doi: 10.3354/cr01204 Clim Res FREEREE ACCESSCCESS Climate classification revisited: from Köppen to Trewartha Michal Belda*, Eva Holtanová, Tomáš Halenka, Jaroslava Kalvová Charles University in Prague, Dept. of Meteorology and Environment Protection, 18200 Prague, Czech Republic ABSTRACT: The analysis of climate patterns can be performed separately for each climatic vari- able or the data can be aggregated, for example, by using a climate classification. These classifi- cations usually correspond to vegetation distribution, in the sense that each climate type is domi- nated by one vegetation zone or eco-region. Thus, climatic classifications also represent a con - venient tool for the validation of climate models and for the analysis of simulated future climate changes. Basic concepts are presented by applying climate classification to the global Climate Research Unit (CRU) TS 3.1 global dataset. We focus on definitions of climate types according to the Köppen-Trewartha climate classification (KTC) with special attention given to the distinction between wet and dry climates. The distribution of KTC types is compared with the original Köp- pen classification (KCC) for the period 1961−1990. In addition, we provide an analysis of the time development of the distribution of KTC types throughout the 20th century. There are observable changes identified in some subtypes, especially semi-arid, savanna and tundra. KEY WORDS: Köppen-Trewartha · Köppen · Climate classification · Observed climate change · CRU TS 3.10.01 dataset · Patton’s dryness criteria Resale or republication not permitted without written consent of the publisher 1. INTRODUCTION The first quantitative classification of Earth’s cli- mate was developed by Wladimir Köppen in 1900 Climate monitoring is mostly based either directly (Kottek et al. -
Climate & Weather Continental Climate with Four Distinct
SOUTH KOREA - COUNTRY FACT SHEET GENERAL INFORMATION Climate & Weather Continental climate with four Time Zone GMT + 9 hours. distinct seasons. Language Korean Currency Won (KRW). Religion Buddhism, Protestantism, International 82 Catholicism, etc. Dialing Code Population About 50 million. Internet Domain .kr Political System Democracy. Emergency 112(Police) Numbers 119(Fire&Medical) Electricity 220 Voltage. Capital City Seoul. What documents Passport & Proof of Please confirm Monthly directly into a Bank required to open employment (after 3days of how salaries are Account. a local Bank arrival). paid? (eg monthly Account? directly into a Can this be done Bank Account) prior to arrival? 1 GENERAL INFORMATION Culture/Business Culture The traditional Confucian social structure is still prevalent. Age and seniority are important and juniors are expected to follow and obey their elders. It is also considered as an important manner at business. Therefore, people often ask you your age and sometimes your marital status to find out their position. These questions are not meant to intrude on one`s privacy. Health care/medical Hospitals and clinics in Korea are generally equipped with the latest treatment medical equipment, and the quality of medical service is quite high as well. Normally, hospitals open from 9 AM to 6 PM, but some hospitals operate a 24-hr emergency medical center offering advice and assistance over the phone and free interpretation service. Education As of May, 2015, there are 56 international schools in Korea: 21 in Seoul, 7 in Gyeonggi-do, 6 in Busan, 4 in Jeju island, and the rest in other provinces or cities. English is the main language in most international schools in Korea, and U.S style curricula are taught. -
Climate Change 2020
Continental AG - Climate Change 2020 C0. Introduction C0.1 (C0.1) Give a general description and introduction to your organization. As of December 31, 2019 the Continental Corporation consists of 581 companies, including non-controlled companies in addition to the parent company Continental AG. The Continental team is made up of 241,458 employees at a total of 595 locations in 59 countries and markets. The postal addresses of companies under our control are defined as locations. Continental has been divided into the group sectors Automotive Technologies, Rubber Technologies and Powertrain Technologies since January 1, 2020. These sectors comprise five business areas with 23 business units. A business area or business unit is classified according to technologies, product groups and services. The business areas and business units have overall responsibility for their business, including their results. Overall responsibility for managing the company is borne by the Executive Board of Continental Aktiengesellschaft (AG). Each business area is represented by one Executive Board member. An exception is the Powertrain business area, which has had its own management since January 1, 2019, following its transformation into an independent legal entity. To ensure a unified business strategy in the Automotive Technologies group sector, the Automotive Board was established on April 1, 2019, with a member of the Executive Board as “spokesman.” The new board is intended to speed up decision-making processes and generate synergies from the closer ties between the Autonomous Mobility and Safety business area and the Vehicle Networking and Information business area. With the exception of Corporate Purchasing, the central functions of Continental AG are represented by the chairman of the Executive Board, the chief financial officer and the Executive Board member responsible for Human Relations. -
Assessing Stack Ventilation Strategies in the Continental Climate of Beijing Using CFD Simulations
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Central Archive at the University of Reading Assessing stack ventilation strategies in the continental climate of Beijing using CFD simulations Emmanuel A Essah a,b, Runming Yao b, Alan Short c a Key Laboratory of the Three Gorges Reservoir Region’s Eco-Environment, Ministry of Education, Chongqing University, China b School of Construction Management and Engineering, University of Reading,Whiteknights, PO Box 219, Reading RG6 6AW, UK c Department of Architecture, University of Cambridge, 1-5 Scroope Terrace, Cambridge CB21PX,UK Abstract The performance of a stack ventilated building compared with two other building designs have been predicted numerically for ventilation and thermal comfort effects in a typical climate of Beijing, China. The buildings were configured based on natural ventilation. Using actual building sizes, Computational Fluid Dynamics (CFD) models were developed, simulated and analysed in Fluent, an ANSYS platform. This paper describes the general design consideration that has been incorporated, the ventilation strategies and the variation in meshing and boundary conditions. The predicted results show that the ventilation flow rates are important parameters to ensure fresh air supply. A Predicted Mean Vote (PMV) model based on ISO-7730 (2005) and the Predicted Percentage Dissatisfied (PPD) indices were simulated using Custom Field Functions (CFF) in the fluent design interface for transition seasons of Beijing. The results showed -
Seasonal Variation of Indoor Radon Concentration Levels in Different
sustainability Article Seasonal Variation of Indoor Radon Concentration Levels in Different Premises of a University Building Pranas Baltrenas˙ 1, Raimondas Grubliauskas 2 and Vaidotas Danila 1,* 1 Research Institute of Environmental Protection, Vilnius Gediminas Technical University, Sauletekis avenue 11, LT-10223 Vilnius, Lithuania; [email protected] 2 Department of Environmental Protection and Water Engineering, Vilnius Gediminas Technical University, Sauletekis avenue 11, LT-10223 Vilnius, Lithuania; [email protected] * Correspondence: [email protected] Received: 25 June 2020; Accepted: 29 July 2020; Published: 31 July 2020 Abstract: In the present study, we aimed to determine the changes of indoor radon concentrations depending on various environmental parameters, such as the outdoor temperature, relative humidity, and air pressure, in university building premises of different applications and heights. The environmental parameters and indoor radon concentrations in four different premises were measured each working day over an eight-month period. The results showed that the indoor radon levels strongly depended on the outside temperature and outside relative humidity, whereas the weakest correlations were found between the indoor radon levels and indoor and outdoor air pressures. The obtained indoor radon concentration and environmental condition correlations were different for the different premises of the building. That is, in two premises where the ventilation effect through unintentional air leakage points prevailed in winter, positive correlations between the radon concentration and outside temperature were obtained, reaching the values of 0.94 and 0.92, respectively. In premises with better airtightness, negative correlations (R = 0.96 and R = 0.62) between the radon concentrations and − − outside temperature were obtained. -
Chapter 6 Climate
Chapter 6 Climate Climate . Canada's climate is not as cold all year around as some may believe. In winter, temperatures fall below freezing point throughout most of Canada. But the south- western coast has a relatively mild climate. Along the Arctic Circle, mean temperatures are below freezing for seven months a year. Climate . During the summer months the southern provinces often experience high levels of humidity and temperatures that can surpass 30 degrees Celsius regularly. Western and south-eastern Canada experience high rainfall, but the Prairies are dry with 250 mm to 500 mm of rain every year. Weather/Climate . Weather – Is the result of the day-to-day conditions of the atmosphere. Climate – A long term pattern of weather – Climate Is The Weather + Weather + More Weather . Climate is what you expect, weather is what you get! Weather . Types of things given in a weather forecast: – Temperature Precipitation – Humidity Wind speed/direction – Cloud cover Air pressure Climate . Factors that affect climate (J.BLOWER); – Jet Stream (air masses) – Bodies of water – Latitude – Ocean Currents – Winds – Elevation – Relief . Note: Different parts of Canada have different climates. Factors that affect Climate A. Jet Stream (Air Masses) Air Masses -- is a large body of air that has similar temperature and moisture properties throughout. For example: Winds blowing from a cold region will bring cold temperature conditions to an area over which they pass Factors that affect Climate . B. Bodies of water – Water warms up more slowly than land and cools off more slowly – As a result of this, land near bodies of water are affected by the weather over these bodies of water.