Applied Hydrometeorology

Size: px
Start display at page:

Download "Applied Hydrometeorology"

Transcription

1 Applied Hydrometeorology

2 Applied Hydrometeorology By Pukh Raj Rakhecha Formerly at Indian Institute of Tropical Meteorology, Pune, India and Vijay P. Singh Department of Biological and Agricultural Engineering and Department of Civil & Environmental Engineering Texas A & M University, College Station, USA

3 A C.I.P. Catalogue record for this book is available from the Library of Congress. ISBN ISBN (HB) (e-book) Copublished by Springer, P.O. Box 17, 3300 AA Dordrecht, The Netherlands with Capital Publishing Company, New Delhi, India. Sold and distributed in North, Central and South America by Springer, 233 Spring Street, New York 10013, USA. In all other countries, except India, sold and distributed by Springer, Haberstrasse 7, D Heidelberg, Germany. In India, sold and distributed by Capital Publishing Company, 7/28, Mahaveer Street, Ansari Road, Daryaganj, New Delhi, , India. Cover photos: Courtesy United States Bureau of Reclamation (USBR) Printed on acid-free paper All Rights Reserved 2009 Capital Publishing Company No part of this work may be reproduced, stored in a retrieval system, or transmitted in any form or by any means, electronic, mechanical, photocopying, microfilming, recording or otherwise, without written permission from the Publisher, with the exception of any material supplied specifically for the purpose of being entered and executed on a computer system, for exclusive use by the purchaser of the work. Printed in India.

4 Dedicated to Our families Wife Anusuya, sons Ashok Kumar and Ramesh Pukh Raj Rakhecha Wife Anita, son Vinay, daughter-in-law Sonali and daughter Arti Vijay P. Singh

5 About the Authors Dr. Pukh Raj Rakhecha, former Dy. Director (Hydrometeorology) with the Indian Institute of Tropical Meteorology in Pune has worked on a variety of hydrometeorological projects including studies of design rainfalls, rainfall statistics, river basin PMP analysis, IFD relations in engineering design, major rainstorms analysis, floods and drought studies, water balance studies and rainfall runoff relations. He has over 250 research papers to his credit and has been consultant on numerous hydrometeorolgical studies. Dr. Rakhecha has travelled widely visiting Australia, Sweden, Switzerland, England, Malaysia, Japan, Iceland and United States for research work and participation in international conferences. He is an internationally recognised hydrometeorologist on PMP studies and member of several scientific societies including International Association of Hydrological Sciences (IAHS). Dr. Vijay P. Singh holds the Caroline & William N Lehrer Distinguished Chair in Water Engineering, is Professor of Civil and Environmental Engineering, and Professor of Biological and Agricultural Engineering at Texas A & M University. He has published more than 450 journal articles, 70 book chapters, 240 conference proceeding papers, and 70 technical reports and bulletins; authored or co-authored fourteen books and has edited another forty-five texts. Prof. Singh has made pioneering contributions in the application of systems analysis, kinematic wave theory, and entropy theory to a range of problems in hydraulics, water quality engineering, irrigation, hydrology and water resources. Prof. Singh has been the recipient of the ASCE Arid Land Hydraulic Engineering Award (2002) and the Ven Te Chow Award (2005), and most recently the AIH Ray K. Linsley Award for outstanding contributions to surface water hydrology. He has served as Editorin-Chief of the Water Science and Technology (WST) series for Springer, and also currently serves as Editor-in-Chief of the ASCE Journal of Hydrologic Engineering and Editor-Chief of Water Science and Engineering. He has directed the organization of 17 international conferences, chaired more than 40 conference sessions, given more than 35 keynote addresses, and examined more than 40 PhD. candidates abroad.

6 Preface Water is vital for life. Since the dawn of civilization, much effort has been made to harness sources of fresh water. Recent years have raised global awareness of the need for increasing demand of water worldwide, largely because of growing population, rising standard of living, higher demand for energy, and greater appreciation for environmental quality. As an example, the world population has increased threefold in the past five decades. In order to meet the rising water demand, water resources are being developed by building large dams, reservoirs, barrages and weirs across rivers worldwide. The guiding principle for water resources development has been to ensure adequate supply of water for agriculture, domestic use (including fine drinking water), waste disposal, industries, and energy production, with due attention to maintain the ecosystem functions. This development, however, depends on a holistic, cooperative and scientific approach. The basic inputs in the assessment of water resources for a given region are from hydrological data and the subject of hydrology forms the core in achieving sustainable development of water resources. Barring a few exceptions, hydrological data for most river basins are sparse and therefore it is difficult to comprehensively assess their water resources. The major source of water is rainfall which occurs as a result of condensation of atmospheric moisture governed by the science of meteorology. Rainfall, therefore, is the principal meteorological element whose recording with other meteorological elements, such as temperature, humidity, wind, and so on, was initiated a long time ago. That is why good networks of raingauge stations have been in existence for several decades in many countries of the world, and long rainfall records are not uncommon these days. Meteorologists, hydrologists and engineers have long recognized the value of hydrometeorological data and more importantly the rainfall data for hydrologic analyses. Thus, application and analysis of meteorological data for the solution of hydrologic problems has precisely come to be known as the science of

7 viii Preface hydrometeorology. In a broad sense, hydrometeorology is a border line science linking meteorology the science of atmosphere with hydrology the science of water of the earth and earth s atmosphere. In engineering hydrology dealing with design and operation of water resource projects, the subject of hydrometeorology occupies a central position. Obviously, the importance of the subject of hydrometeorology has become increasingly recognized and it is now studied not only by hydrologists and engineers but also by students from many different disciplines. Realizing the importance of the subject, there is a need for a textbook like the present one on applied hydrometeorology oriented towards the Asian environment, particularly to India, which can provide a complete set of tools to practicing engineers and hydrologists engaged in the planning, development and management of water resources. This constitutes the primary objective of this book. The emphasis in the book is on the practical applications of meteorology for water resources development and understanding of the needed meteorological concepts. The subject matter of the book follows this rationale. The book contains 15 chapters encompassing a wide spectrum of topics of hydrometeorology. Chapter 1 scopes out the area of hydrometeorology, and deals with meteorological variables and their use in hydrology, hydrological cycle, global distribution of land and water, and global water budget. Chapter 2 discusses the earth-atmospheric system. Included in the discussion are composition of the atmosphere, mass of atmosphere and hydrosphere, vertical structure of atmosphere, air density and its variation, hydrostatic equation, hydrostatics of special atmosphere, reduction of pressure to sea level, and atmospheric stability. The discussion of meteorological processes, constituting the subject matter of Chapter 3, includes compression and expansion of gases, forms of heat, equation of state for a perfect gas, isothermal and adiabatic changes, the first law of thermodynamics, adiabatic process, vertical motion in the atmosphere, mixture of gases, equation of state of moist air, and precipitable water. Chapter 4 deals with radiation and temperature. Beginning with a discussion of the source of heat and light, it goes on to discuss different aspects of radiation, mean annual heat balance, non-radiative heat exchange between the earth and the troposphere, heat balance, and temperature zones. Weather systems for precipitation are discussed in Chapter 5. Included in the discussion are pressure belts; wind systems of the earth; and scales of weather systems including planetary scale, synoptic scale, and meso scale of weather systems. Chapter 6 deals with weather and precipitation in India. The discussion in the chapter includes location and area, land forms, river basins, and seasons of India; climate controls; rainfall and runoff of continents; seasonal variation of pressure and temperature; onset and withdrawal of monsoons; weather systems affecting Indian rainfall; history of rainfall measurement in India; rainfall over India; assessment of rainwater resources; and present status of water utilization in India.

8 Preface ix Defining and classifying tropical disturbances and hurricanes, Chapter 7 discusses major hurricanes and super typhoons, wind rotation, conversion of wind speeds, formation of tropical storms, frequency of hurricanes for oceanic regions, absence of hurricanes in South Atlantic Ocean, naming hurricanes, life cycle of hurricanes, structure of hurricanes, hurricane climatology, record hurricane, largest rainfall from tropical storms/hurricanes, longest lasting hurricanes, climatic effects of hurricane activity, global warming and hurricanes, hurricane threats, damages and destruction, seeding of hurricanes, and damage caused by cyclones. Greatest point and areal rainfalls constitute the subject matter of Chapter 8. It includes significant point rainfall occurrences over India, China, Australia, and Japan; world s greatest point rainfalls; importance of greatest areal rainfalls; and greatest areal rainfalls over India, USA, Japan, and China. Recognizing rainfall as an important source of input for water resources, Chapter 9 covers precipitation and its measurement. It also encompasses mechanisms of precipitation, forms of precipitation, types of precipitation, measurement of precipitation, network design, estimation of missing data, mean depth of rainfall over an area, consistency of rainfall records, extension and interpretation of rainfall data, intensity-duration relationships, and point rainfall and areal rainfall relationships. The physical evaluation of probable maximum precipitation (PMP) based on a hydrometeorological procedure is a topic of considerable importance in designing large dams, reservoirs, and spillways and for the derivation of probable maximum floods (PMF). Techniques for estimating the PMP constitute the subject matter of Chapter 9. They discuss rainstorm analysis, depth-area-duration analysis, design storm, data for design storm studies, methods of estimating design storms, probable maximum precipitation, and methods of estimating PMP. Chapter 10 deals with design storm estimation. The material contained in this chapter is of particular value to design engineers. The discussion includes rainstorm and its analysis, depth-area-duration analysis of a rainstorm, design storms, data for design storm studies, methods for estimating design storms, probable maximum precipitation, and methods of estimating PMP. Statistical analysis of precipitation is presented in Chapter 11. It deals with data series for frequency analysis, recurrence interval, calculated risk, frequency analysis, measures of central tendency, measures of variability, skewness, and kurtosis (flattening), moments of frequency distribution, standard frequency distributions, tests of significance, homogeneity of data series, and frequency analysis. Foreshadowing rainfall is covered in Chapter 12. It includes measures of variability, correlation analysis, global scale factors affecting rainfall, types of weather forecasts, techniques for long-range rainfall forecasting in India, Indian summer monsoon and southern oscillation index, statistical techniques used in long range forecasting, multiple regression analysis, and parameters in long-range forecasting of Indian summer monsoon rainfall.

9 x Preface Chapter 13 deals with evaporation. Beginning with a discussion of the physics of evaporation, it goes on to discuss factors affecting evaporation, measurement of evaporation, evaporation measurement in India, and estimation of evaporation by indirect methods. Extreme hydrometeorological events that arise from unusually high and low precipitation lead to floods and droughts, respectively. These events cause considerable loss of life and property. Droughts constitute the subject matter of Chapter 14. It discusses causes of droughts, evapotranspiration and potential evapotranspiration, types of droughts, droughts in India, El Nino factor relating to droughts, and absence of tropical disturbances and Indian rainfall. The concluding chapter, Chapter 15, is on floods. Defining floods and classifying them, the chapter goes on to discuss the kinds and causes of floods, effects of floods, flood measurements, flood control, estimation of peak floods, flood frequency analysis, floods in Indian rivers, highest floods in India, and comparison of highest floods in India with world s highest floods. The text material of each chapter contains illustrative examples, which are mostly based on actual, recorded data. It is hoped that the book will be of much use to the professionals engaged in water resources planning, development, and management. Also the book should be useful to university courses concerned with hydrometeorology and its application to water-related issues, as it caters to the requirement of the syllabi of various Indian and foreign universities. There is vast literature on the topics in this book. A comprehensive list of references has been advertently omitted, and only those studies that are deemed most pertinent have been cited. This is because the intended audience would be more interested in applications rather than advanced literature. This, however, in no way reflects a lack of appreciation for the literature. Indeed this book would not have been completed without reviewing the pertinent literature. We have tried to make our acknowledgments as specific as possible. We would be most grateful if readers discovering any discrepancies, errors, or misprints would bring them to our attention. Our families provided unwavering support and help, without which this book would not have been completed. As a small token of our appreciation for their love and support, we dedicate this book to them. January 2009 Pukh Raj Rakhecha Vijay P. Singh

10 Contents About the Authors Preface vi vii 1. Introduction Scope of Hydrometeorology Meteorological Variables Earth System Orbital Motion of Earth and Seasons Global Distribution of Land and Water Global Water Budget Hydrologic Cycle 20 References The Atmosphere Earth-atmosphere System Composition of the Atmosphere Mass of the Atmosphere and the Hydrosphere Average Vertical Structure of Atmosphere Hydrostatic Equation Hydrostatics of Special Atmosphere Reduction of Pressure to Sea Level Atmospheric Stability and Instability 37 References Atmospheric Processes Heat and Temperature Compression and Expansion of a Gas Forms of Heat Equation of State for a Gas: Perfect Gas 41

11 xii Contents 3.5 Isothermal and Adiabatic Changes First Law of Thermodynamics Vertical Motion in the Atmosphere Mixture of Gases Equation of State of Moist Air Precipitable Water 50 References Radiation and Temperature Sun: The Source of Heat and Light Radiation Laws of Radiation Incoming Solar Radiation without Atmosphere at the Earth s Surface Passage of Solar Radiation through Average Atmospheric Condition Terrestrial Radiation Mean Annual Heat Balance of the Earth-Atmosphere System Non-radiative Heat Exchange between the Earth and the Troposphere Heat Balance Temperature Zones 68 References Weather Systems for Precipitation Pressure Belts and Wind Systems of the Earth Scale of Weather Systems Planetary Scale Weather Systems Synoptic Scale Weather Systems Meso Scale Weather Systems Oceanic Circulation 87 References Weather and Precipitation in India Location and Area of India Land Forms of India Climatic Control River Basins of India Rainfall and Runoff of Continents The Seasons of India Seasonal Variation of Pressure Mean Seasonal Variation of Air Temperature Onset and Withdrawal of Monsoons Main Weather Systems Affecting Indian Rainfall 111

12 Contents xiii 6.11 History of Rainfall Measurement in India Rainfall over India Assessment of Rainwater Resources of India Present Status of Water Utilization in India 122 References Tropical Storms and Hurricanes Definition Major Hurricanes and Super Typhoons Wind Rotation Formation of Tropical Storms Origin of Hurricanes Frequency of Hurricanes for Oceanic Regions Absence of Hurricanes in South Atlantic Ocean Naming of Hurricanes Life Cycle of Hurricanes Structure of Hurricanes Hurricane Climatology Most Intense Hurricanes on Record Largest Rainfall from Tropical Storms/Hurricanes Longest Lasting Hurricanes Climatic Effects of Hurricane Activity Global Warming and Hurricanes Hurricane Threats, Damage and Destruction 157 References Greatest Point and Areal Rainfalls Definitions Significant Rainfall Occurrences over India Significant Rainfall Occurrences over China Significant Rainfall Occurrences over Australia Significant Rainfall Occurrences over Japan World's Greatest Point Rainfalls Importance of the Greatest Areal Rainfalls Greatest Areal Rainfalls over India Greatest Areal Rainfalls over the USA Greatest Areal Rainfalls over China Greatest Areal Rainfalls over Australia 188 References Precipitation and Its Measurement Mechanisms of Precipitation Forms of Precipitation Types of Precipitation Measurement of Precipitation 194

13 xiv Contents 9.5 Network Design Estimation of Missing Rainfall Mean Depth of Rainfall Over an Area Consistency of Rainfall Records Extension and Interpretation of Rainfall Data Intensity-Duration Relationships Point Rainfall to Areal Rainfall Relationship 216 References Design Storm Estimation Rainstorm and its Analysis Depth-area-duration Analysis of a Rainstorm Design Storm Data for Design Storm Studies Methods for Estimating Design Storms Probable Maximum Precipitation Methods of Estimating PMP 230 References Statistical Analysis of Precipitation Data Series for Frequency Analysis Recurrence Interval Calculated Risk Frequency Analysis Measures of Central Tendency Measures of Variability Measures of Skewness Measure of Kurtosis (Flattening) Moments of Frequency Distribution Standard Frequency Distributions Homogeneity of Data Empirical Frequency Analysis Frequency Analysis by the Gumbel Method Frequency Factors 276 References Foreshadowing Precipitation Correlation Analysis Measure of Variability Global Scale Factors Affecting Rainfall Types of Weather Forecasts Development of Long Range Forecast of Rainfall in India Indian Summer Monsoon and Southern Oscillation Index Statistical Techniques in Long Range Forecast based on Improved Parameters 293

14 Contents xv 12.8 Multiple Regression Analysis Required Parameters in Long-range Forecasting of Indian Summer Monsoon Rainfall 297 References Evaporation Physics of Evaporation Factors Affecting Evaporation Measurement of Evaporation Evaporation Measurement in India Estimation of Evaporation by Indirect Methods 305 References Droughts Causes of Droughts Evapotranspiration and Potential Evapotranspiration Types of Droughts Droughts in India El Nino Factor Relating to Droughts Absence of Tropical Disturbances and Indian Rainfall 337 References Floods Definition of Flood Kinds of Floods Causes of Floods Effects of Floods Surface Runoff and Runoff Process Runoff Measurements Hydrograph Flood Control Estimation of Peak Flood Floods in Indian Rivers Highest Floods in India Comparison of the Highest Floods in India with World s Highest Floods 373 References 375 Appendix: World Weather Extremes 377 Index 379

ENTROPY-BASED PARAMETER ESTIMATION IN HYDROLOGY

ENTROPY-BASED PARAMETER ESTIMATION IN HYDROLOGY ENTROPY-BASED PARAMETER ESTIMATION IN HYDROLOGY Water Science and Technology Library VOLUME 30 Editor-in-Chief V. P. Singh, Louisiana State University, Baton Rouge, U.S.A Editorial Advisory Board M. Anderson,

More information

Principles of Agricultural Meteorology

Principles of Agricultural Meteorology Principles of Agricultural Meteorology About the Author Balaji Mohan Mote was born on 9 th September 1988 at Ambajogai, Dist- Beed (Maharashtra). He has obtained B.Sc. (Ag.) degree from Dr. Panjabrao Deshmukh

More information

What a Hurricane Needs to Develop

What a Hurricane Needs to Develop Massive Storms! Hurricanes What a Hurricane Needs to Develop Warm tropical water - at least 80 F High Humidity Light wind Low Pressure Area Form between 5 and 20 latitude Hurricane Ingredients Hurricane

More information

ESCI 110: 2 s.h. Introduction to Earth Sciences Programs ESCI 322: 3 s.h. Environmental Hydrology ESCI 241: 4 s.h. Meteorology (G2, L)

ESCI 110: 2 s.h. Introduction to Earth Sciences Programs ESCI 322: 3 s.h. Environmental Hydrology ESCI 241: 4 s.h. Meteorology (G2, L) ESCI 110: 2 s.h. Introduction to Earth Sciences Programs General introduction to each of the earth sciences disciplines and to college life. 2 hrs. lec. Offered in fall. Restricted to earth sciences majors.

More information

Respiration in Archaea and Bacteria

Respiration in Archaea and Bacteria Respiration in Archaea and Bacteria Advances in Photosynthesis and Respiration VOLUME 16 Series Editor: GOVINDJEE University of Illinois, Urbana, Illinois, U.S.A. Consulting Editors: Christine FOYER, Harpenden,

More information

Climate Change in the Pacific: Scientific Assessment and New Research Volume 1: Regional Overview

Climate Change in the Pacific: Scientific Assessment and New Research Volume 1: Regional Overview Climate Change in the Pacific: Scientific Assessment and New Research Volume 1: Regional Overview Australian Bureau of Meteorology and Commonwealth Scientific and Industrial Research Organisation (CSIRO)

More information

Graduate Courses Meteorology / Atmospheric Science UNC Charlotte

Graduate Courses Meteorology / Atmospheric Science UNC Charlotte Graduate Courses Meteorology / Atmospheric Science UNC Charlotte In order to inform prospective M.S. Earth Science students as to what graduate-level courses are offered across the broad disciplines of

More information

1990 Intergovernmental Panel on Climate Change Impacts Assessment

1990 Intergovernmental Panel on Climate Change Impacts Assessment 1990 Intergovernmental Panel on Climate Change Impacts Assessment Although the variability of weather and associated shifts in the frequency and magnitude of climate events were not available from the

More information

Solution: The ratio of normal rainfall at station A to normal rainfall at station i or NR A /NR i has been calculated and is given in table below.

Solution: The ratio of normal rainfall at station A to normal rainfall at station i or NR A /NR i has been calculated and is given in table below. 3.6 ESTIMATION OF MISSING DATA Data for the period of missing rainfall data could be filled using estimation technique. The length of period up to which the data could be filled is dependent on individual

More information

Advances in Photosynthesis and Respiration

Advances in Photosynthesis and Respiration Plant Respiration Advances in Photosynthesis and Respiration VOLUME 18 Series Editor: GOVINDJEE University of Illinois, Urbana, Illinois, U.S.A. Consulting Editors: Christine FOYER, Harpenden, U.K. Elisabeth

More information

MPACT OF EL-NINO ON SUMMER MONSOON RAINFALL OF PAKISTAN

MPACT OF EL-NINO ON SUMMER MONSOON RAINFALL OF PAKISTAN MPACT OF EL-NINO ON SUMMER MONSOON RAINFALL OF PAKISTAN Abdul Rashid 1 Abstract: El-Nino is the dominant mod of inter- annual climate variability on a planetary scale. Its impact is associated worldwide

More information

THE STUDY OF NUMBERS AND INTENSITY OF TROPICAL CYCLONE MOVING TOWARD THE UPPER PART OF THAILAND

THE STUDY OF NUMBERS AND INTENSITY OF TROPICAL CYCLONE MOVING TOWARD THE UPPER PART OF THAILAND THE STUDY OF NUMBERS AND INTENSITY OF TROPICAL CYCLONE MOVING TOWARD THE UPPER PART OF THAILAND Aphantree Yuttaphan 1, Sombat Chuenchooklin 2 and Somchai Baimoung 3 ABSTRACT The upper part of Thailand

More information

Springer Atmospheric Sciences

Springer Atmospheric Sciences Springer Atmospheric Sciences More information about this series at http://www.springer.com/series/10176 Ewa Łupikasza The Climatology of Air- Mass and Frontal Extreme Precipitation Study of meteorological

More information

Weather & Ocean Currents

Weather & Ocean Currents Weather & Ocean Currents Earth is heated unevenly Causes: Earth is round Earth is tilted on an axis Earth s orbit is eliptical Effects: Convection = vertical circular currents caused by temperature differences

More information

School Name Team # International Academy East Meteorology Test Graphs, Pictures, and Diagrams Diagram #1

School Name Team # International Academy East Meteorology Test Graphs, Pictures, and Diagrams Diagram #1 School Name Team # International Academy East Meteorology Test Graphs, Pictures, and Diagrams Diagram #1 Use the map above, and the locations marked A-F, to answer the following questions. 1. The center

More information

Fluid Circulation Review. Vocabulary. - Dark colored surfaces absorb more energy.

Fluid Circulation Review. Vocabulary. - Dark colored surfaces absorb more energy. Fluid Circulation Review Vocabulary Absorption - taking in energy as in radiation. For example, the ground will absorb the sun s radiation faster than the ocean water. Air pressure Albedo - Dark colored

More information

Massive Storms! 8.10C Identify the role of the oceans in the formation of weather systems such as hurricanes

Massive Storms! 8.10C Identify the role of the oceans in the formation of weather systems such as hurricanes Massive Storms! 8.10C Identify the role of the oceans in the formation of weather systems such as hurricanes Instructional page: Each person in group will take on one portion or set of questions: Each

More information

ENGINEERING MECHANICS

ENGINEERING MECHANICS ENGINEERING MECHANICS Engineering Mechanics Volume 2: Stresses, Strains, Displacements by C. HARTSUIJKER Delft University of Technology, Delft, The Netherlands and J.W. WELLEMAN Delft University of Technology,

More information

Topic 6: Insolation and the Seasons

Topic 6: Insolation and the Seasons Topic 6: Insolation and the Seasons Solar Radiation and Insolation Insolation: In Sol ation The Sun is the primary source of energy for the earth. The rate at which energy is radiated is called Intensity

More information

Comparison of physical and statistical methods for estimating probable maximum precipitation in southwestern basins of Iran

Comparison of physical and statistical methods for estimating probable maximum precipitation in southwestern basins of Iran Fattahi et al. / DESERT 15 (2010) 127-132 DESERT DESERT Online at http://jdesert.ut.ac.ir DESERT 15 (2010) 127-132 Comparison of physical and statistical methods for estimating probable maximum precipitation

More information

Energy Systems, Structures and Processes Essential Standard: Analyze patterns of global climate change over time Learning Objective: Differentiate

Energy Systems, Structures and Processes Essential Standard: Analyze patterns of global climate change over time Learning Objective: Differentiate Energy Systems, Structures and Processes Essential Standard: Analyze patterns of global climate change over time Learning Objective: Differentiate between weather and climate Global Climate Focus Question

More information

East Penn School District Curriculum and Instruction

East Penn School District Curriculum and Instruction East Penn School District Curriculum and Instruction Curriculum for: Meteorology Course(s): Meteorology Grades: 10-12 Department: Science Length of Period (average minutes): 42 Periods per cycle: 6 Length

More information

CHAPTER 13 WEATHER ANALYSIS AND FORECASTING MULTIPLE CHOICE QUESTIONS

CHAPTER 13 WEATHER ANALYSIS AND FORECASTING MULTIPLE CHOICE QUESTIONS CHAPTER 13 WEATHER ANALYSIS AND FORECASTING MULTIPLE CHOICE QUESTIONS 1. The atmosphere is a continuous fluid that envelops the globe, so that weather observation, analysis, and forecasting require international

More information

Climate and the Atmosphere

Climate and the Atmosphere Climate and Biomes Climate Objectives: Understand how weather is affected by: 1. Variations in the amount of incoming solar radiation 2. The earth s annual path around the sun 3. The earth s daily rotation

More information

Fundamentals of Weather and Climate

Fundamentals of Weather and Climate Fundamentals of Weather and Climate ROBIN McILVEEN Environmental Science Division Institute of Environmental and Biological Sciences Lancaster University CHAPMAN & HALL London Glasgow Weinheim New York

More information

Photosynthetic Rate and Dynamic Environment

Photosynthetic Rate and Dynamic Environment Photosynthetic Rate and Dynamic Environment Photosynthetic Rate and Dynamic Environment by Kazutoshi Yabuki Professor Emeritus, Osaka Prefecture University, Sakai, Japan SPRINGER-SCIENCE+BUSINESS MEDIA,

More information

Science 1206 Chapter 1 - Inquiring about Weather

Science 1206 Chapter 1 - Inquiring about Weather Science 1206 Chapter 1 - Inquiring about Weather 1.1 - The Atmosphere: Energy Transfer and Properties (pp. 10-25) Weather and the Atmosphere weather the physical conditions of the atmosphere at a specific

More information

What a Hurricane Needs to Develop

What a Hurricane Needs to Develop Weather Weather is the current atmospheric conditions, such as air temperature, wind speed, wind direction, cloud cover, precipitation, relative humidity, air pressure, etc. 8.10B: global patterns of atmospheric

More information

SEMESTER AT SEA COURSE SYLLABUS. Earth s Weather and Climate EVSC 1300

SEMESTER AT SEA COURSE SYLLABUS. Earth s Weather and Climate EVSC 1300 1 COURSE DESCRIPTION SEMESTER AT SEA COURSE SYLLABUS Earth s Weather and Climate EVSC 1300 Our voyage takes us through a variety of climatic zones giving us the opportunity to observe the atmosphere in

More information

Bell Work. REVIEW: Our Planet Earth Page 29 Document A & B Questions

Bell Work. REVIEW: Our Planet Earth Page 29 Document A & B Questions 9.12.16 Bell Work REVIEW: Our Planet Earth Page 29 Document A & B Questions Intro to Climate & Weather https://www.youtube.com/watch?v=vhgyoa70q7y Weather vs. Climate Video Climate & Weather 3.1 Weather

More information

CHAPTER 6 Air-Sea Interaction Pearson Education, Inc.

CHAPTER 6 Air-Sea Interaction Pearson Education, Inc. CHAPTER 6 Air-Sea Interaction Chapter Overview The atmosphere and the ocean are one independent system. Earth has seasons because of the tilt on its axis. There are three major wind belts in each hemisphere.

More information

Haiti and Dominican Republic Flash Flood Initial Planning Meeting

Haiti and Dominican Republic Flash Flood Initial Planning Meeting Dr Rochelle Graham Climate Scientist Haiti and Dominican Republic Flash Flood Initial Planning Meeting September 7 th to 9 th, 2016 Hydrologic Research Center http://www.hrcwater.org Haiti and Dominican

More information

Marine Ecoregions. Marine Ecoregions. Slide 1. Robert G. Bailey. USDA Forest Service Rocky Mountain Research Station

Marine Ecoregions. Marine Ecoregions. Slide 1. Robert G. Bailey. USDA Forest Service Rocky Mountain Research Station Slide 1 Marine Ecoregions Robert G. Bailey Marine Ecoregions Robert G. Bailey USDA Forest Service Rocky Mountain Research Station rgbailey@fs.fed.us Draft of 7/20/2006 8:44 PM Abstract: Oceans occupy some

More information

Ocean in Motion 7: El Nino and Hurricanes!

Ocean in Motion 7: El Nino and Hurricanes! Ocean in Motion 7: El Nino and Hurricanes! A. Overview 1. Ocean in Motion -- El Nino and hurricanes We will look at the ocean-atmosphere interactions that cause El Nino and hurricanes. Using vocabulary

More information

El Niño / Southern Oscillation

El Niño / Southern Oscillation El Niño / Southern Oscillation Student Packet 2 Use contents of this packet as you feel appropriate. You are free to copy and use any of the material in this lesson plan. Packet Contents Introduction on

More information

Untitled.notebook May 12, Thunderstorms. Moisture is needed to form clouds and precipitation the lifting of air, or uplift, must be very strong

Untitled.notebook May 12, Thunderstorms. Moisture is needed to form clouds and precipitation the lifting of air, or uplift, must be very strong Thunderstorms Moisture is needed to form clouds and precipitation the lifting of air, or uplift, must be very strong cold air and warm air must mix; creating an active circulation system that has both

More information

South Asian Climate Outlook Forum (SASCOF-6)

South Asian Climate Outlook Forum (SASCOF-6) Sixth Session of South Asian Climate Outlook Forum (SASCOF-6) Dhaka, Bangladesh, 19-22 April 2015 Consensus Statement Summary Below normal rainfall is most likely during the 2015 southwest monsoon season

More information

Anticipated and Observed Trends in the Global Hydrological Cycle. Kevin E. Trenberth NCAR

Anticipated and Observed Trends in the Global Hydrological Cycle. Kevin E. Trenberth NCAR Anticipated and Observed Trends in the Global Hydrological Cycle Kevin E. Trenberth NCAR The presence of moisture affects the disposition of incoming solar radiation: Evaporation (drying) versus temperature

More information

Climate Changes due to Natural Processes

Climate Changes due to Natural Processes Climate Changes due to Natural Processes 2.6.2a Summarize natural processes that can and have affected global climate (particularly El Niño/La Niña, volcanic eruptions, sunspots, shifts in Earth's orbit,

More information

US Drought Status. Droughts 1/17/2013. Percent land area affected by Drought across US ( ) Dev Niyogi Associate Professor Dept of Agronomy

US Drought Status. Droughts 1/17/2013. Percent land area affected by Drought across US ( ) Dev Niyogi Associate Professor Dept of Agronomy Droughts US Drought Status Dev Niyogi Associate Professor Dept of Agronomy Deptof Earth Atmospheric Planetary Sciences Indiana State Climatologist Purdue University LANDSURFACE.ORG iclimate.org climate@purdue.edu

More information

Introduction to Climatology. GEOG/ENST 2331: Lecture 1

Introduction to Climatology. GEOG/ENST 2331: Lecture 1 Introduction to Climatology GEOG/ENST 2331: Lecture 1 Us Graham Saunders graham.saunders@lakeheadu.ca Jason Freeburn (RC 2004) jtfreebu@lakeheadu.ca Graham Saunders Australian Weather Bureau Environment

More information

Lecture 2: Light And Air

Lecture 2: Light And Air Lecture 2: Light And Air Earth s Climate System Earth, Mars, and Venus Compared Solar Radiation Greenhouse Effect Thermal Structure of the Atmosphere Atmosphere Ocean Solid Earth Solar forcing Land Energy,

More information

Earth and Space Science. Teacher s Guide

Earth and Space Science. Teacher s Guide Earth and Space Science Teacher s Guide WALCH PUBLISHING Table of Contents To the Teacher............................................................. vi Classroom Management....................................................

More information

Enantiomer Separation

Enantiomer Separation Enantiomer Separation Enantiomer Separation Fundamentals and Practical Methods Edited by Professor of Chemistry, Department of Chemistry, Okayama University of Science, Japan KLUWER ACADEMIC PUBLISHERS

More information

Stochastic Hydrology. a) Data Mining for Evolution of Association Rules for Droughts and Floods in India using Climate Inputs

Stochastic Hydrology. a) Data Mining for Evolution of Association Rules for Droughts and Floods in India using Climate Inputs Stochastic Hydrology a) Data Mining for Evolution of Association Rules for Droughts and Floods in India using Climate Inputs An accurate prediction of extreme rainfall events can significantly aid in policy

More information

The Global Scope of Climate. The Global Scope of Climate. Keys to Climate. Chapter 8

The Global Scope of Climate. The Global Scope of Climate. Keys to Climate. Chapter 8 The Global Scope of Climate Chapter 8 The Global Scope of Climate In its most general sense, climate is the average weather of a region, but except where conditions change very little during the course

More information

THE OPEN UNIVERSITY OF SRI LANKA

THE OPEN UNIVERSITY OF SRI LANKA THE OPEN UNIVERSITY OF SRI LANKA Extended Abstracts Open University Research Sessions (OURS 2017) 16 th & 17 th November, 2017 The Open University of Sri Lanka - 2017 All rights reserved. No part of this

More information

Detailed Syllabus in Geography for B.A/ B. Sc Semester- III under CBCS for the Examination to be held in December 2017, 2018 and 2019

Detailed Syllabus in Geography for B.A/ B. Sc Semester- III under CBCS for the Examination to be held in December 2017, 2018 and 2019 Detailed Syllabus in Geography for B.A/ B. Sc Semester- III under CBCS for the Examination to be held in December 2017, 2018 and 2019 Course Code: UGOTC- 301 (Theory Core) Title: Physical Geography- II

More information

ATMOSPHERIC MODELLING. GEOG/ENST 3331 Lecture 9 Ahrens: Chapter 13; A&B: Chapters 12 and 13

ATMOSPHERIC MODELLING. GEOG/ENST 3331 Lecture 9 Ahrens: Chapter 13; A&B: Chapters 12 and 13 ATMOSPHERIC MODELLING GEOG/ENST 3331 Lecture 9 Ahrens: Chapter 13; A&B: Chapters 12 and 13 Agenda for February 3 Assignment 3: Due on Friday Lecture Outline Numerical modelling Long-range forecasts Oscillations

More information

Thermodynamics of Atmospheres and Oceans

Thermodynamics of Atmospheres and Oceans Thermodynamics of Atmospheres and Oceans Judith A. Curry and Peter J. Webster PROGRAM IN ATMOSPHERIC AND OCEANIC SCIENCES DEPARTMENT OF AEROSPACE ENGINEERING UNIVERSITY OF COLORADO BOULDER, COLORADO USA

More information

CERTAIN ASPECTS OF THE NUMERICAL SIMULATION OF CIRCULATION IN THE BAY OF BENGAL AND THE ARABIAN SEA

CERTAIN ASPECTS OF THE NUMERICAL SIMULATION OF CIRCULATION IN THE BAY OF BENGAL AND THE ARABIAN SEA CERTAIN ASPECTS OF THE NUMERICAL SIMULATION OF CIRCULATION IN THE BAY OF BENGAL AND THE ARABIAN SEA by INDU JAIN A THESIS SUBMITTED IN FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY

More information

Climate Outlook through 2100 South Florida Ecological Services Office Vero Beach, FL September 9, 2014

Climate Outlook through 2100 South Florida Ecological Services Office Vero Beach, FL September 9, 2014 Climate Outlook through 2100 South Florida Ecological Services Office Vero Beach, FL September 9, 2014 Short Term Drought Map: Short-term (

More information

Introduction to Climatology. GEOG/ENST 2331: Lecture 1

Introduction to Climatology. GEOG/ENST 2331: Lecture 1 Introduction to Climatology GEOG/ENST 2331: Lecture 1 Us! Graham Saunders (RC 2006C) graham.saundersl@lakeheadu.ca! Jason Freeburn (RC 2004) jtfreebu@lakeheadu.ca Graham Saunders! Australian Weather Bureau!

More information

Climate Dynamics (PCC 587): Hydrologic Cycle and Global Warming

Climate Dynamics (PCC 587): Hydrologic Cycle and Global Warming Climate Dynamics (PCC 587): Hydrologic Cycle and Global Warming D A R G A N M. W. F R I E R S O N U N I V E R S I T Y O F W A S H I N G T O N, D E P A R T M E N T O F A T M O S P H E R I C S C I E N C

More information

p = ρrt p = ρr d = T( q v ) dp dz = ρg

p = ρrt p = ρr d = T( q v ) dp dz = ρg Chapter 1: Properties of the Atmosphere What are the major chemical components of the atmosphere? Atmospheric Layers and their major characteristics: Troposphere, Stratosphere Mesosphere, Thermosphere

More information

Chapter-1 Introduction

Chapter-1 Introduction Modeling of rainfall variability and drought assessment in Sabarmati basin, Gujarat, India Chapter-1 Introduction 1.1 General Many researchers had studied variability of rainfall at spatial as well as

More information

Wind: Global Systems Chapter 10

Wind: Global Systems Chapter 10 Wind: Global Systems Chapter 10 General Circulation of the Atmosphere General circulation of the atmosphere describes average wind patterns and is useful for understanding climate Over the earth, incoming

More information

Lecture 8: Natural Climate Variability

Lecture 8: Natural Climate Variability Lecture 8: Natural Climate Variability Extratropics: PNA, NAO, AM (aka. AO), SAM Tropics: MJO Coupled A-O Variability: ENSO Decadal Variability: PDO, AMO Unforced vs. Forced Variability We often distinguish

More information

Unit: Weather Study Guide

Unit: Weather Study Guide Name: Period: Unit: Weather Study Guide Define each vocabulary word on a separate piece of paper or index card. Weather Climate Temperature Wind chill Heat index Sky conditions UV index Visibility Wind

More information

2013 Summer Weather Outlook. Temperatures, Precipitation, Drought, Hurricanes and why we care

2013 Summer Weather Outlook. Temperatures, Precipitation, Drought, Hurricanes and why we care 2013 Summer Weather Outlook Temperatures, Precipitation, Drought, Hurricanes and why we care Role of the ERCOT Meteorologist Forecasts Develop temperature input for hourly load forecasts (next day, days

More information

Atmospheric Moisture, Precipitation, and Weather Systems

Atmospheric Moisture, Precipitation, and Weather Systems Atmospheric Moisture, Precipitation, and Weather Systems 6 Chapter Overview The atmosphere is a complex system, sometimes described as chaotic in nature. In this chapter we examine one of the principal

More information

Study of Hydrometeorology in a Hard Rock Terrain, Kadirischist Belt Area, Anantapur District, Andhra Pradesh

Study of Hydrometeorology in a Hard Rock Terrain, Kadirischist Belt Area, Anantapur District, Andhra Pradesh Open Journal of Geology, 2012, 2, 294-300 http://dx.doi.org/10.4236/ojg.2012.24028 Published Online October 2012 (http://www.scirp.org/journal/ojg) Study of Hydrometeorology in a Hard Rock Terrain, Kadirischist

More information

SEASONAL CLIMATE OUTLOOK VALID FOR JULY-AUGUST- SEPTEMBER 2013 IN WEST AFRICA, CHAD AND CAMEROON

SEASONAL CLIMATE OUTLOOK VALID FOR JULY-AUGUST- SEPTEMBER 2013 IN WEST AFRICA, CHAD AND CAMEROON SEASONAL CLIMATE OUTLOOK VALID FOR JULY-AUGUST- SEPTEMBER 2013 IN WEST AFRICA, CHAD AND CAMEROON May 29, 2013 ABUJA-Federal Republic of Nigeria 1 EXECUTIVE SUMMARY Given the current Sea Surface and sub-surface

More information

Chapter 9 External Energy Fuels Weather and Climate

Chapter 9 External Energy Fuels Weather and Climate Natural Disasters Tenth Edition Chapter 9 External Energy Fuels Weather and Climate Copyright The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 9-1 Weather Versus Climate

More information

Colorado State University (CSU) Atlantic Hurricane Season Forecast

Colorado State University (CSU) Atlantic Hurricane Season Forecast Colorado State University (CSU) Atlantic Hurricane Season Forecast Dr. Philip Klotzbach of Colorado State University (CSU) has issued his April forecast for the 2018 Atlantic Hurricane Season. The forecast

More information

Long term weather trends in Phaltan, Maharashtra. French intern at NARI, student from Ecole Centrale de Lyon, Ecully 69130, France.

Long term weather trends in Phaltan, Maharashtra. French intern at NARI, student from Ecole Centrale de Lyon, Ecully 69130, France. Long term weather trends in Phaltan, Maharashtra A. Jacob and Anil K. Rajvanshi French intern at NARI, student from Ecole Centrale de Lyon, Ecully 693, France. Director NARI, Nimbkar Agricultural Research

More information

ENGINEERING HYDROLOGY

ENGINEERING HYDROLOGY ENGINEERING HYDROLOGY Prof. Rajesh Bhagat Asst. Professor Civil Engineering Department Yeshwantrao Chavan College Of Engineering Nagpur B. E. (Civil Engg.) M. Tech. (Enviro. Engg.) GCOE, Amravati VNIT,

More information

Recent development of the National Hydro-Meteorological Service (NHMS) of Viet Nam for disaster risk reduction

Recent development of the National Hydro-Meteorological Service (NHMS) of Viet Nam for disaster risk reduction Ministry of Natural Resources and Environment National Hydro-Meteorological Service Recent development of the National Hydro-Meteorological Service (NHMS) of Viet Nam for disaster risk reduction Tran Van

More information

EL NINO-SOUTHERN OSCILLATION (ENSO): RECENT EVOLUTION AND POSSIBILITIES FOR LONG RANGE FLOW FORECASTING IN THE BRAHMAPUTRA-JAMUNA RIVER

EL NINO-SOUTHERN OSCILLATION (ENSO): RECENT EVOLUTION AND POSSIBILITIES FOR LONG RANGE FLOW FORECASTING IN THE BRAHMAPUTRA-JAMUNA RIVER Global NEST Journal, Vol 8, No 3, pp 79-85, 2006 Copyright 2006 Global NEST Printed in Greece. All rights reserved EL NINO-SOUTHERN OSCILLATION (ENSO): RECENT EVOLUTION AND POSSIBILITIES FOR LONG RANGE

More information

Climate Modeling: From the global to the regional scale

Climate Modeling: From the global to the regional scale Climate Modeling: From the global to the regional scale Filippo Giorgi Abdus Salam ICTP, Trieste, Italy ESA summer school on Earth System Monitoring and Modeling Frascati, Italy, 31 July 11 August 2006

More information

Best track data of tropical cyclonic disturbances. over the north Indian Ocean. Regional Specialised Meteorological Centre (RSMC) -

Best track data of tropical cyclonic disturbances. over the north Indian Ocean. Regional Specialised Meteorological Centre (RSMC) - Best track data of tropical cyclonic disturbances over the north Indian Ocean Regional Specialised Meteorological Centre (RSMC) - Tropical Cyclones, New Delhi Cyclone Warning Division, India Meteorological

More information

Name the surface winds that blow between 0 and 30. GEO 101, February 25, 2014 Monsoon Global circulation aloft El Niño Atmospheric water

Name the surface winds that blow between 0 and 30. GEO 101, February 25, 2014 Monsoon Global circulation aloft El Niño Atmospheric water GEO 101, February 25, 2014 Monsoon Global circulation aloft El Niño Atmospheric water Name the surface winds that blow between 0 and 30 What is the atmospheric pressure at 0? What is the atmospheric pressure

More information

ATMOSPHERIC SCIENCE-ATS (ATS)

ATMOSPHERIC SCIENCE-ATS (ATS) Atmospheric Science-ATS (ATS) 1 ATMOSPHERIC SCIENCE-ATS (ATS) Courses ATS 150 Science of Global Climate Change Credits: 3 (3-0-0) Physical basis of climate change. Energy budget of the earth, the greenhouse

More information

SIXTH INTERNATIONAL WORKSHOP on TROPICAL CYCLONES

SIXTH INTERNATIONAL WORKSHOP on TROPICAL CYCLONES WMO/CAS/WWW SIXTH INTERNATIONAL WORKSHOP on TROPICAL CYCLONES Topic 4a : Updated Statement on the Possible Effects of Climate Change on Tropical Cyclone Activity/Intensity Rapporteur: E-mail: John McBride

More information

Spatial Variability of Aerosol - Cloud Interactions over Indo - Gangetic Basin (IGB)

Spatial Variability of Aerosol - Cloud Interactions over Indo - Gangetic Basin (IGB) Spatial Variability of Aerosol - Cloud Interactions over Indo - Gangetic Basin (IGB) Shani Tiwari Graduate School of Environmental Studies Nagoya University, Nagoya, Japan Email: pshanitiwari@gmail.com

More information

Chapter 1. Introduction: What drives the ocean currents?

Chapter 1. Introduction: What drives the ocean currents? Chapter 1 Introduction: What drives the ocean currents? Sixty years ago, this textbook would have been titled "Introductory Geography of the Oceans". Physical oceanography then was a close relative of

More information

CLIM-111/PHYS-111 Introduction to the Fundamentals of Atmospheric Science CLIM-112/PHYS-112 Lab

CLIM-111/PHYS-111 Introduction to the Fundamentals of Atmospheric Science CLIM-112/PHYS-112 Lab CLIM-111/PHYS-111 Introduction to the Fundamentals of Atmospheric Science CLIM-112/PHYS-112 Lab An overview of the Earth s atmosphere, its history, and the fundamental physical and chemical processes which

More information

Extreme Weather Events and Climate Change

Extreme Weather Events and Climate Change Extreme Weather Events and Climate Change Robert M Rabin NOAA/National Severe Storms Lab Norman, Oklahoma Most material presented is from: Climate Change 2013: The Physical Science Basis. Intergovernmental

More information

Weather Outlook 2016: Cycles and Patterns Influencing Our Growing Season

Weather Outlook 2016: Cycles and Patterns Influencing Our Growing Season Weather Outlook 2016: Cycles and Patterns Influencing Our Growing Season Leon F. Osborne Chester Fritz Distinguished Professor of Atmospheric Sciences University of North Dakota Cycle of El Niño Events

More information

Weather Forecasts and Climate AOSC 200 Tim Canty. Class Web Site: Lecture 27 Dec

Weather Forecasts and Climate AOSC 200 Tim Canty. Class Web Site:   Lecture 27 Dec Weather Forecasts and Climate AOSC 200 Tim Canty Class Web Site: http://www.atmos.umd.edu/~tcanty/aosc200 Topics for today: Climate Natural Variations Feedback Mechanisms Lecture 27 Dec 4 2018 1 Climate

More information

Vertical wind shear in relation to frequency of Monsoon Depressions and Tropical Cyclones of Indian Seas

Vertical wind shear in relation to frequency of Monsoon Depressions and Tropical Cyclones of Indian Seas Vertical wind shear in relation to frequency of Monsoon Depressions and Tropical Cyclones of Indian Seas Prince K. Xavier and P.V. Joseph Department of Atmospheric Sciences Cochin University of Science

More information

Advanced Hydrology. (Web course)

Advanced Hydrology. (Web course) Advanced Hydrology (Web course) Subhankar Karmakar Assistant Professor Centre for Environmental Science and Engineering (CESE) Indian Institute of Technology Bombay Powai, Mumbai 400 076 Email: skarmakar@iitb.ac.in

More information

Assessing Land Surface Albedo Bias in Models of Tropical Climate

Assessing Land Surface Albedo Bias in Models of Tropical Climate DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Assessing Land Surface Albedo Bias in Models of Tropical Climate William R. Boos (PI) Yale University PO Box 208109 New

More information

Analysis of Rainfall and Other Weather Parameters under Climatic Variability of Parbhani ( )

Analysis of Rainfall and Other Weather Parameters under Climatic Variability of Parbhani ( ) International Journal of Current Microbiology and Applied Sciences ISSN: 2319-7706 Volume 7 Number 06 (2018) Journal homepage: http://www.ijcmas.com Original Research Article https://doi.org/10.20546/ijcmas.2018.706.295

More information

Components of the Climate System. Lecture 2: Earth s Climate System. Pop Quiz. Sub-components Global cycles What comes in What goes out

Components of the Climate System. Lecture 2: Earth s Climate System. Pop Quiz. Sub-components Global cycles What comes in What goes out Lecture 2: Earth s Climate System Components of the Climate System terrestrial radiation Atmosphere Ocean solar radiation Land Energy, Water, and Biogeochemistry Cycles Sub-components Global cycles What

More information

Climate Outlook through 2100 South Florida Ecological Services Office Vero Beach, FL January 13, 2015

Climate Outlook through 2100 South Florida Ecological Services Office Vero Beach, FL January 13, 2015 Climate Outlook through 2100 South Florida Ecological Services Office Vero Beach, FL January 13, 2015 Short Term Drought Map: Short-term (

More information

Estimating Probable Maximum Precipitation for Linau River Basin in Sarawak

Estimating Probable Maximum Precipitation for Linau River Basin in Sarawak Estimating Probable Maximum Precipitation for Linau River Basin in Sarawak M. Hussain, S. Nadya and F.J. Chia Hydropower Development Division, Sarawak Energy Berhad, 93050, Kuching, Sarawak, Malaysia Date

More information

Operational Monsoon Monitoring at NCEP

Operational Monsoon Monitoring at NCEP Operational Monsoon Monitoring at NCEP Wassila M. Thiaw Climate Prediction Center National Centers for Environmental Predictions Operational Monsoon Monitoring at NCEP Wassila M. Thiaw Climate Prediction

More information

FINAL EXAM PRACTICE #3: Meteorology, Climate, and Ecology

FINAL EXAM PRACTICE #3: Meteorology, Climate, and Ecology FINAL EXAM PRACTICE #3: Meteorology, Climate, and Ecology 1. Clay is watching the weather to prepare for a trip to the beach tomorrow. The forecast predicts that a low-pressure system will move in overnight.

More information

DEVELOPMENT OF MAXIMUM AVERAGE RAINFALL INTENSITY RELATIONSHIPS WITH 24 HOUR AVERAGE RAINFALL INTENSITY

DEVELOPMENT OF MAXIMUM AVERAGE RAINFALL INTENSITY RELATIONSHIPS WITH 24 HOUR AVERAGE RAINFALL INTENSITY International Journal of Civil Engineering and Technology (IJCIET) Volume 8, Issue, June, pp., Article ID: IJCIET_8 Available online at http://www.ia aeme.com/ijciet/issues.asp?jtype=ijciet&vtyp pe=8&itype=

More information

Introduction to tropical meteorology and deep convection

Introduction to tropical meteorology and deep convection Introduction to tropical meteorology and deep convection TMD Lecture 1 Roger K. Smith University of Munich A satpix tour of the tropics The zonal mean circulation (Hadley circulation), Inter- Tropical

More information

Lecture 2: Earth s Climate System

Lecture 2: Earth s Climate System Lecture 2: Earth s Climate System terrestrial radiation solar radiation Atmosphere Ocean Solid Earth Land Energy, Water, and Biogeochemistry Cycles Sub-components Global cycles What comes in What goes

More information

At the Midpoint of the 2008

At the Midpoint of the 2008 At the Midpoint of the 2008 Atlantic Hurricane Season Editor s note: It has been an anxious couple of weeks for those with financial interests in either on- or offshore assets in the Gulf of Mexico and

More information

Creating a WeatherSMART nation: SAWS drought related research, services and products

Creating a WeatherSMART nation: SAWS drought related research, services and products Creating a WeatherSMART nation: SAWS drought related research, services and products Drought Dialogue 23-24 June 2016 Western Cape Government Hannes Rautenbach South African Weather Service SAWS mandate

More information

Tokyo Climate Center Website (TCC website) and its products -For monitoring the world climate and ocean-

Tokyo Climate Center Website (TCC website) and its products -For monitoring the world climate and ocean- Tokyo, 14 November 2016, TCC Training Seminar Tokyo Climate Center Website (TCC website) and its products -For monitoring the world climate and ocean- Yasushi MOCHIZUKI Tokyo Climate Center Japan Meteorological

More information

What is the IPCC? Intergovernmental Panel on Climate Change

What is the IPCC? Intergovernmental Panel on Climate Change IPCC WG1 FAQ What is the IPCC? Intergovernmental Panel on Climate Change The IPCC is a scientific intergovernmental body set up by the World Meteorological Organization (WMO) and by the United Nations

More information

Climate Change 2007: The Physical Science Basis

Climate Change 2007: The Physical Science Basis Climate Change 2007: The Physical Science Basis Working Group I Contribution to the IPCC Fourth Assessment Report Presented by R.K. Pachauri, IPCC Chair and Bubu Jallow, WG 1 Vice Chair Nairobi, 6 February

More information

A High Resolution Daily Gridded Rainfall Data Set ( ) for Mesoscale Meteorological Studies

A High Resolution Daily Gridded Rainfall Data Set ( ) for Mesoscale Meteorological Studies National Climate Centre Research Report No: 9/2008 A High Resolution Daily Gridded Rainfall Data Set (1971-2005) for Mesoscale Meteorological Studies M. Rajeevan and Jyoti Bhate National Climate Centre

More information

Patterns of summer rainfall variability across tropical Australia - results from EOT analysis

Patterns of summer rainfall variability across tropical Australia - results from EOT analysis 18 th World IMACS / MODSIM Congress, Cairns, Australia 13-17 July 29 http://mssanz.org.au/modsim9 Patterns of summer rainfall variability across tropical Australia - results from EOT analysis Smith, I.N.

More information

Possible Applications of Deep Neural Networks in Climate and Weather. David M. Hall Assistant Research Professor Dept. Computer Science, CU Boulder

Possible Applications of Deep Neural Networks in Climate and Weather. David M. Hall Assistant Research Professor Dept. Computer Science, CU Boulder Possible Applications of Deep Neural Networks in Climate and Weather David M. Hall Assistant Research Professor Dept. Computer Science, CU Boulder Quick overview of climate and weather models Weather models

More information