Chile extends from tropics down almost to Antarctica and is located on the west side of the Andes
|
|
|
- Patience Daniel
- 7 years ago
- Views:
Transcription
1 UNDP Climate Change Country Profiles Chile A. Karmalkar 1, C. McSweeney 1, M. New 1,2 and G. Lizcano 1 1. School of Geography and Environment, University of Oxford. 2. Tyndall Centre for Climate Change Research General Climate Chile extends from tropics down almost to Antarctica and is located on the west side of the Andes M E - S conditions. The north of the country experiences very hot and arid conditions (Atacama Desert) whereas the climate in central Chile is Mediterranean, with cool, wet winters between April and S A C C C I me south the weather is cold and wet most of the year. Annual rainfall ranges from no recorded precipitation in some of the north to mm in south-central Chile, to more than 4000 mm in some southern regions. The most important factors that control the climate in Chile are the Pacific Anticyclone, the southern circumpolar low pressure area, the cold Humboldt Current, and the Andes Mountains. The Humboldt Current together with the prevailing south-westerly winds creates a temperate climate in most of northern and central Chile, even in areas that lie in tropical latitudes. Recent Climate Trends Temperature Mean annual temperature does not show significant trend in Chile since Mean SON C 1960, at an average rate of C The frequency of hot nights has increased significantly since 1960 in every season. T C 5.6% of nights) between 1960 and The rate of increase is very similar in all seasons.
2 Chile Precipitation No significant change has been observed in mean rainfall over Chile since The proportion of rainfall falling in heavy events has decreased by 2.2% annually between 1960 and GCM Projections of Future Climate Temperature T C C T C o The projected rate of warming is similar throughout the year, but warming is C C and southern Chile. All projections indicate substantial increases in the frequency of days and nights that are 1 in current climate. o A -26% of days by the 2060s, and 20-37% of days by the 2090s. o N -99 are projected to occur on 15-26% of nights by the 2060s and 18-38% of nights by the 2090s. Nights that are hot for each season are projected to increase most rapidly in DJF, occurring on 26-61% of nights by the 2090s. All projections indicate decreases in the frequency of days and nights that are considered 2 in current climate. Precipitation Projections of mean annual rainfall from different models in the ensemble are broadly consistent in indicating decreases in rainfall for Chile. Ensemble median values for all seasons are negative. o Annual projections vary between -5 to +2% by the 2090s with ensemble median changes of -3 to -5% when averaged over the entire country. o Projected decrease is significantly higher in central Chile S seasons and is over 40% by the 2090s in SON under the A2 scenario. 1 H ays or nights in current climate of that region and season. 2 C of that region or season.
3 Chile The proportion of total rainfall that falls in heavy 3 events shows very small or no change in the model projections. Maximum 1- and 5-day rainfalls do not show any consistent change in model projections under the future scenarios. Additional Regional Climate Change Information Complex topography in this part of the world means that local variations in response to global warming, particularly precipitation, are likely to be large and many areas may vary from the regional trend (Christensen et al., 2007). The course resolution of the GCMs is also inadequate to capture local variations in climate of Chile due to its complex topography and elongated shape. For further information see Christensen et al. IPCC W G I The P S B, Chapter 11 (Regional Climate projections): Sections 11.6 (South and Central America). 3 A H ily rainfall total which exceeds the threshold that is exceeded on 5% of rainy days in current the climate of that region and season.
4 Chile Data Summary Observed Mean Observed Trend Projected changes by the Projected changes by the 2060s Projected changes by the 2030s 2090s Min Median Max Min Median Max Min Median Max Temperature C (change in C decade) C C C C C C A Annual A1B B A DJF A1B B A MAM A1B B A JJA A1B B A SON * A1B B Precipitation (mm per month) (change in mm per decade) Change in mm per month Change in mm per month Change in mm per month A Annual A1B B A DJF A1B B A MAM A1B B A JJA A1B B A SON A1B B Precipitation (%) (mm per month) (change in % per decade) % Change % Change % Change A Annual A1B B A DJF A1B B A MAM A1B B A JJA A1B B A SON A1B B
5 Chile Observed Mean Observed Trend Projected changes by the Projected changes by the 2060s Projected changes by the 2030s 2090s Min Median Max Min Median Max Min Median Max % Frequency Change in frequency per decade Future % frequency Future % frequency Frequency of Hot Days (TX90p) A2 **** **** **** Annual A1B **** **** **** B1 **** **** **** A2 **** **** **** DJF A1B **** **** **** B1 **** **** **** A2 **** **** **** MAM A1B **** **** **** B1 **** **** **** A2 **** **** **** JJA A1B **** **** **** B1 **** **** **** A2 **** **** **** SON A1B **** **** **** B1 **** **** **** Frequency of Hot Nights (TN90p) A2 **** **** **** Annual * A1B **** **** **** B1 **** **** **** A2 **** **** **** DJF * A1B **** **** **** B1 **** **** **** A2 **** **** **** MAM * A1B **** **** **** B1 **** **** **** A2 **** **** **** JJA * A1B **** **** **** B1 **** **** **** A2 **** **** **** SON * A1B **** **** **** B1 **** **** **** Frequency of Cold Days (TX10p) A2 **** **** **** Annual A1B **** **** **** B1 **** **** **** A2 **** **** **** DJF A1B **** **** **** B1 **** **** **** A2 **** **** **** MAM A1B **** **** **** B1 **** **** **** A2 **** **** **** JJA A1B **** **** **** B1 **** **** **** A2 **** **** **** SON A1B **** **** **** B1 **** **** **** Frequency of Cold Nights (TN10p) A2 **** **** **** Annual * A1B **** **** **** B1 **** **** **** A2 **** **** **** DJF * A1B **** **** **** B1 **** **** **** A2 **** **** **** MAM * A1B **** **** **** B1 **** **** **** A2 **** **** **** JJA * A1B **** **** **** B1 **** **** **** A2 **** **** **** SON * A1B **** **** **** B1 **** **** ****
6 Chile Observed Mean Observed Trend Projected changes by the 2030s Projected changes by the 2060s Projected changes by the 2090s Min Median Max Min Median Max Min Median Max % total rainfall falling in Heavy Events (R95pct) % Change in % per decade Change in % Change in % A2 **** **** **** Annual * A1B **** **** **** B1 **** **** **** A2 **** **** **** DJF **** **** A1B **** **** **** B1 **** **** **** A2 **** **** **** MAM **** **** A1B **** **** **** B1 **** **** **** A2 **** **** **** JJA **** **** A1B **** **** **** B1 **** **** **** A2 **** **** **** SON **** **** A1B **** **** **** B1 **** **** **** Maximum 1-day rainfall (RX1day) mm Change in mm per decade Change in mm Change in mm A2 **** **** **** Annual **** **** A1B **** **** **** B1 **** **** **** A2 **** **** **** DJF A1B **** **** **** B1 **** **** **** A2 **** **** **** MAM * A1B **** **** **** B1 **** **** **** A2 **** **** **** JJA A1B **** **** **** B1 **** **** **** A2 **** **** **** SON A1B **** **** **** B1 **** **** **** Maximum 5-day Rainfall (RX5day) mm Change in mm per decade Change in mm Change in mm A2 **** **** **** Annual A1B **** **** **** B1 **** **** **** A2 **** **** **** DJF A1B **** **** **** B1 **** **** **** A2 **** **** **** MAM A1B **** **** **** B1 **** **** **** A2 **** **** **** JJA A1B **** **** **** B1 **** **** **** A2 **** **** **** SON A1B **** **** **** B1 **** **** **** * indicates trend is statistically significant at 95% confidence **** indicates data are not available
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
24
25
26
South Africa. General Climate. UNDP Climate Change Country Profiles. A. Karmalkar 1, C. McSweeney 1, M. New 1,2 and G. Lizcano 1
UNDP Climate Change Country Profiles South Africa A. Karmalkar 1, C. McSweeney 1, M. New 1,2 and G. Lizcano 1 1. School of Geography and Environment, University of Oxford. 2. Tyndall Centre for Climate
What Causes Climate? Use Target Reading Skills
Climate and Climate Change Name Date Class Climate and Climate Change Guided Reading and Study What Causes Climate? This section describes factors that determine climate, or the average weather conditions
Socio-Economic Impacts of Climate Change in Afghanistan Executive Summary
Socio-Economic Impacts of Climate Change in Afghanistan Executive Summary CNTR- 08 8507 DFID CNTR 08 8507 Executive Summary Socio-Economic Impacts of Climate Change in Afghanistan A Report to the Department
ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 9 May 2011
ENSO Cycle: Recent Evolution, Current Status and Predictions Update prepared by Climate Prediction Center / NCEP 9 May 2011 Outline Overview Recent Evolution and Current Conditions Oceanic Niño Index (ONI)
Monsoon Variability and Extreme Weather Events
Monsoon Variability and Extreme Weather Events M Rajeevan National Climate Centre India Meteorological Department Pune 411 005 rajeevan@imdpune.gov.in Outline of the presentation Monsoon rainfall Variability
The IPCC Special Report on Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation
The IPCC Special Report on Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation A changing climate leads to changes in extreme weather and climate events 2 How do changes
Current climate change scenarios and risks of extreme events for Northern Europe
Current climate change scenarios and risks of extreme events for Northern Europe Kirsti Jylhä Climate Research Finnish Meteorological Institute (FMI) Network of Climate Change Risks on Forests (FoRisk)
Queensland rainfall past, present and future
Queensland rainfall past, present and future Historically, Queensland has had a variable climate, and recent weather has reminded us of that fact. After experiencing the longest drought in recorded history,
Regionalizing global models:
Regionalizing global models: value-adding for impacts and adaptation Jason Evans University of New South Wales Yann Arthus-Bertrand / Altitude Regionalizing Global models Why would we want to regionalize
CLIMATE, WATER & LIVING PATTERNS THINGS
CLIMATE, WATER & LIVING PATTERNS NAME THE SIX MAJOR CLIMATE REGIONS DESCRIBE EACH CLIMATE REGION TELL THE FIVE FACTORS THAT AFFECT CLIMATE EXPLAIN HOW THOSE FACTORS AFFECT CLIMATE DESCRIBE HOW CLIMATES
SEA START Climate Change Analysis Tool v1.1
SEA START Climate Change Analysis Tool v1.1 SEA START RC has developed tool to aid data analysis for the future climate data which is downloaded from Climate Data Distribution System (http://cc.start.or.th).
How To Predict Climate Change
A changing climate leads to changes in extreme weather and climate events the focus of Chapter 3 Presented by: David R. Easterling Chapter 3:Changes in Climate Extremes & their Impacts on the Natural Physical
Guy Carpenter Asia-Pacific Climate Impact Centre, School of energy and Environment, City University of Hong Kong
Diurnal and Semi-diurnal Variations of Rainfall in Southeast China Judy Huang and Johnny Chan Guy Carpenter Asia-Pacific Climate Impact Centre School of Energy and Environment City University of Hong Kong
Seasonal & Daily Temperatures. Seasons & Sun's Distance. Solstice & Equinox. Seasons & Solar Intensity
Seasonal & Daily Temperatures Seasons & Sun's Distance The role of Earth's tilt, revolution, & rotation in causing spatial, seasonal, & daily temperature variations Please read Chapter 3 in Ahrens Figure
Update from Reto and Erich
Update from Reto and Erich From theory and models to observations Erich Fischer and Reto Knutti ETH Zurich, Switzerland Schematic illustrating precipitation changes Where does it come from? After CCSP
WEATHER AND CLIMATE practice test
WEATHER AND CLIMATE practice test Multiple Choice Identify the choice that best completes the statement or answers the question. 1. What role does runoff play in the water cycle? a. It is the process in
Present trends and climate change projections for the Mediterranean region
Present trends and climate change projections for the Mediterranean region Prof. Piero Lionello, piero.lionello@unile.it Science of Materials Department, University of Salento, Italy Plan of the talk:
2. The map below shows high-pressure and low-pressure weather systems in the United States.
1. Which weather instrument has most improved the accuracy of weather forecasts over the past 40 years? 1) thermometer 3) weather satellite 2) sling psychrometer 4) weather balloon 6. Wind velocity is
defined largely by regional variations in climate
1 Physical Environment: Climate and Biomes EVPP 110 Lecture Instructor: Dr. Largen Fall 2003 2 Climate and Biomes Ecosystem concept physical and biological components of environment are considered as single,
ENSO: Recent Evolution, Current Status and Predictions. Update prepared by: Climate Prediction Center / NCEP 29 June 2015
ENSO: Recent Evolution, Current Status and Predictions Update prepared by: Climate Prediction Center / NCEP 29 June 2015 Outline Summary Recent Evolution and Current Conditions Oceanic Niño Index (ONI)
6. Base your answer to the following question on the graph below, which shows the average monthly temperature of two cities A and B.
1. Which single factor generally has the greatest effect on the climate of an area on the Earth's surface? 1) the distance from the Equator 2) the extent of vegetative cover 3) the degrees of longitude
Selecting members of the QUMP perturbed-physics ensemble for use with PRECIS
Selecting members of the QUMP perturbed-physics ensemble for use with PRECIS Isn t one model enough? Carol McSweeney and Richard Jones Met Office Hadley Centre, September 2010 Downscaling a single GCM
CLIMATE OF RWANDA. Overview. Linked to other lessons
Geography S6 GENERAL PHYSICAL GEOGRAPHY OF RWANDA Lesson 75 Developed by (Niwagaba Innocent) Subtopic Climate and factors influencing it in Rwanda Specific Objectives The learners must be able to: Describe
Chapter 3 Communities, Biomes, and Ecosystems
Communities, Biomes, and Ecosystems Section 1: Community Ecology Section 2: Terrestrial Biomes Section 3: Aquatic Ecosystems Click on a lesson name to select. 3.1 Community Ecology Communities A biological
THE ECOSYSTEM - Biomes
Biomes The Ecosystem - Biomes Side 2 THE ECOSYSTEM - Biomes By the end of this topic you should be able to:- SYLLABUS STATEMENT ASSESSMENT STATEMENT CHECK NOTES 2.4 BIOMES 2.4.1 Define the term biome.
WEATHER, CLIMATE AND ADAPTATIONS OF ANIMALS TO CLIMATE
7 WEATHER, CLIMATE AND ADAPTATIONS OF ANIMALS TO CLIMATE TEXTBOOK QUESTIONS AND ANSWERS Q.1. Why weather changes so frequently? Ans. All changes in the weather are caused by the sun. The movement of the
FLOOD FORECASTING PRACTICE IN NORTHERN CALIFORNIA
FLOOD FORECASTING PRACTICE IN NORTHERN CALIFORNIA California Department of Water Resources Post Office Box 219000, Sacramento, California 95821 9000 USA By Maurice Roos, Chief Hydrologist ABSTRACT Although
Physiography, Geography and Climate of Latin America (Lecture 3)
Physiography, Geography and Climate of Latin America (Lecture 3) Natural Landmarks in Latin America World's longest and second highest mountain range, and the world's highest active volcanoes. Biggest
Climate Extremes Research: Recent Findings and New Direc8ons
Climate Extremes Research: Recent Findings and New Direc8ons Kenneth Kunkel NOAA Cooperative Institute for Climate and Satellites North Carolina State University and National Climatic Data Center h#p://assessment.globalchange.gov
WEATHER LIMITATIONS FOR WINTER AND SUMMER TOURISM IN EUROPE. K. Blazejczyk Institute of Geography and Spatial Organization, Polish Academy of Science
Developments in Tourism Climatology A. Matzarakis, C. R. de Freitas, D. Scott, 27 WEATHER LIMITATIONS FOR WINTER AND SUMMER TOURISM IN EUROPE K. Blazejczyk Institute of Geography and Spatial Organization,
sample The IPCC Special Report on Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation
sample The IPCC Special Report on Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation A changing climate leads to changes in extreme weather and climate events 2 Impacts
Chapter Overview. Seasons. Earth s Seasons. Distribution of Solar Energy. Solar Energy on Earth. CHAPTER 6 Air-Sea Interaction
Chapter Overview CHAPTER 6 Air-Sea Interaction 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.
1. Incredible India. Shade the map on the next page, to show India s relief. The correct shading is shown on the final page! Incredible India India
1. Incredible India Shade the map on the next page, to show India s relief. The correct shading is shown on the final page! Incredible India India The DCSF supported Action plan for Geography is delivered
Geography affects climate.
KEY CONCEPT Climate is a long-term weather pattern. BEFORE, you learned The Sun s energy heats Earth s surface unevenly The atmosphere s temperature changes with altitude Oceans affect wind flow NOW, you
Regional climate change experiments over southern South America. II: Climate change scenarios in the late twenty-first century
Clim Dyn DOI 10.1007/s00382-008-0449-8 Regional climate change experiments over southern South America. II: Climate change scenarios in the late twenty-first century Mario N. Nuñez Æ Silvina A. Solman
IGAD CLIMATE PREDICTION AND APPLICATION CENTRE
IGAD CLIMATE PREDICTION AND APPLICATION CENTRE CLIMATE WATCH REF: ICPAC/CW/No.32 May 2016 EL NIÑO STATUS OVER EASTERN EQUATORIAL OCEAN REGION AND POTENTIAL IMPACTS OVER THE GREATER HORN OF FRICA DURING
Temporal variation in snow cover over sea ice in Antarctica using AMSR-E data product
Temporal variation in snow cover over sea ice in Antarctica using AMSR-E data product Michael J. Lewis Ph.D. Student, Department of Earth and Environmental Science University of Texas at San Antonio ABSTRACT
climate science A SHORT GUIDE TO This is a short summary of a detailed discussion of climate change science.
A SHORT GUIDE TO climate science This is a short summary of a detailed discussion of climate change science. For more information and to view the full report, visit royalsociety.org/policy/climate-change
A simple scaling approach to produce climate scenarios of local precipitation extremes for the Netherlands
Supplementary Material to A simple scaling approach to produce climate scenarios of local precipitation extremes for the Netherlands G. Lenderink and J. Attema Extreme precipitation during 26/27 th August
CGC1D1: Interactions in the Physical Environment Factors that Affect Climate
Name: Date: Day/Period: CGC1D1: Interactions in the Physical Environment Factors that Affect Climate Chapter 12 in the Making Connections textbook deals with Climate Connections. Use pages 127-144 to fill
Armenian State Hydrometeorological and Monitoring Service
Armenian State Hydrometeorological and Monitoring Service Offenbach 1 Armenia: IN BRIEF Armenia is located in Southern Caucasus region, bordering with Iran, Azerbaijan, Georgia and Turkey. The total territory
Noon Sun Angle = 90 Zenith Angle
Noon Sun Angle Worksheet Name Name Date Subsolar Point (Latitude where the sun is overhead at noon) Equinox March 22 nd 0 o Equinox September 22 nd 0 o Solstice June 22 nd 23.5 N Solstice December 22 nd
Full name:.. Date:. School: Teacher: Contents:
Contents: 1.- The atmosphere. 2.- Weather and climate. 3.- The elements of climate 3.1 Temperatures 3.2 Rainfalls 3.3 Atmospheric pressure 3.4 Wind 4.-The Natural Environment. Full name:.. Date:. Class:
Water Conservation and Drainage of Golf
Golf Course Environmental Profile Phase II, Volume I Water Use and Conservation Practices on U.S. Golf Courses Funded by the USGA through the Environmental Institute for Golf, the philanthropic organization
Climate Change Impacts in the Asia/Pacific Region
Climate Change Impacts in the Asia/Pacific Region Global CC threat CC in the A/P region The Stern Review and IPCC 4 th Assessment Report both state that climate change will have adverse impact on people
Local Climate Changes: present and future
Local Climate Changes: present and future Rodica Rodica Tomozeiu Tomozeiu Lucio Lucio Botarelli Botarelli www.arpa.emr.it www.arpa.emr.it Global climate changes Increase Increase of of the the global global
Climates are described by the same conditions used to describe
58 The Causes of Climate R E A D I N G Climates are described by the same conditions used to describe weather, such as temperature, precipitation, and wind. You now know that oceans have an important effect
Climate Ready Tools & Resources
August 2, 2013 Mission Statement To provide the water sector (drinking water, wastewater, and stormwater utilities) with the practical tools, training, and technical assistance needed to adapt to climate
ENVIRONMENTAL STRUCTURE AND FUNCTION: CLIMATE SYSTEM Vol. II - Low-Latitude Climate Zones and Climate Types - E.I. Khlebnikova
LOW-LATITUDE CLIMATE ZONES AND CLIMATE TYPES E.I. Khlebnikova Main Geophysical Observatory, St. Petersburg, Russia Keywords: equatorial continental climate, ITCZ, subequatorial continental (equatorial
Regional Climate Projections
11 Coordinating Lead Authors: Jens Hesselbjerg Christensen (Denmark), Bruce Hewitson (South Africa) Lead Authors: Aristita Busuioc (Romania), Anthony Chen (Jamaica), Xuejie Gao (China), Isaac Held (USA),
8.5 Comparing Canadian Climates (Lab)
These 3 climate graphs and tables of data show average temperatures and precipitation for each month in Victoria, Winnipeg and Whitehorse: Figure 1.1 Month J F M A M J J A S O N D Year Precipitation 139
The Pennsylvania Observer
The Pennsylvania Observer August 3, 2009 July 2009 - Pennsylvania Weather Recap Written by: Dan DePodwin After a cool month of June, some hoped July would bring usual summertime warmth to the state of
How To Predict Climate Change In Tonga
Niuatoputapu Niuafo'ou Late Island Vava u Group South Pacific Ocean Tofua Island Kotu Group Nomuka Group Ha apai Group NUKU ALOFA Eua Island Tongatapu Group Current and future climate of Tonga > Tonga
AWESOME ADAPTATIONS WORKSHEETS. for. Rainforest Desert Mediterranean
AWESOME ADAPTATIONS WORKSHEETS for Rainforest Desert Mediterranean IN THE RAINFOREST Write a sentence to record your experience in the Tropical House IT FEELS. IT SMELLS. THE TEMPERATURE is IT MAKES ME
7.10 INCORPORATING HYDROCLIMATIC VARIABILITY IN RESERVOIR MANAGEMENT AT FOLSOM LAKE, CALIFORNIA
7.10 INCORPORATING HYDROCLIMATIC VARIABILITY IN RESERVOIR MANAGEMENT AT FOLSOM LAKE, CALIFORNIA Theresa M. Carpenter 1, Konstantine P. Georgakakos 1,2, Nicholas E. Graham 1,2, Aris P. Georgakakos 3,4,
Seasonal Temperature Variations
Seasonal and Daily Temperatures Fig. 3-CO, p. 54 Seasonal Temperature Variations What causes the seasons What governs the seasons is the amount of solar radiation reaching the ground What two primary factors
Climate of Illinois Narrative Jim Angel, state climatologist. Introduction. Climatic controls
Climate of Illinois Narrative Jim Angel, state climatologist Introduction Illinois lies midway between the Continental Divide and the Atlantic Ocean, and the state's southern tip is 500 miles north of
The Polar Climate Zones
The Polar Climate Zones How cold is it in the polar climate? Polar areas are the coldest of all the major climate zones The Sun is hardly ever high enough in the sky to cause the plentiful ice to melt,
ES 106 Laboratory # 3 INTRODUCTION TO OCEANOGRAPHY. Introduction The global ocean covers nearly 75% of Earth s surface and plays a vital role in
ES 106 Laboratory # 3 INTRODUCTION TO OCEANOGRAPHY 3-1 Introduction The global ocean covers nearly 75% of Earth s surface and plays a vital role in the physical environment of Earth. For these reasons,
Lecture 4: Pressure and Wind
Lecture 4: Pressure and Wind Pressure, Measurement, Distribution Forces Affect Wind Geostrophic Balance Winds in Upper Atmosphere Near-Surface Winds Hydrostatic Balance (why the sky isn t falling!) Thermal
The Influence of the Climatic Peculiarities on the Electromagnetic Waves Attenuation in the Baltic Sea Region
PIERS ONLINE, VOL. 4, NO. 3, 2008 321 The Influence of the Climatic Peculiarities on the Electromagnetic Waves Attenuation in the Baltic Sea Region M. Zilinskas 1,2, M. Tamosiunaite 2,3, S. Tamosiunas
Parametric Analysis of School Classroom Typologies' Energy Performance
PLEA2013-29th Conference, Sustainable Architecture for a Renewable Future, Munich, Germany 10-12 September 2013 Parametric Analysis of School Classroom Typologies' Energy Performance MAUREEN TREBILCOCK
REGIONAL CLIMATE AND DOWNSCALING
REGIONAL CLIMATE AND DOWNSCALING Regional Climate Modelling at the Hungarian Meteorological Service ANDRÁS HORÁNYI (horanyi( horanyi.a@.a@met.hu) Special thanks: : Gabriella Csima,, Péter Szabó, Gabriella
California Standards Grades 9 12 Boardworks 2009 Science Contents Standards Mapping
California Standards Grades 912 Boardworks 2009 Science Contents Standards Mapping Earth Sciences Earth s Place in the Universe 1. Astronomy and planetary exploration reveal the solar system s structure,
Climate Change in Mexico implications for the insurance and reinsurance market
Climate Change in Mexico implications for the insurance and reinsurance market Eberhard Faust Geo Risks Research Munich Reinsurance Company 1980 April 2008: Billion & Ten Billion Dollar Losses The costliest
The Global Distribution of Mineral Dust
The Global Distribution of Mineral Dust Ina Tegen Leibniz Institute for f r Tropospheric ric Research, Leipzig, Germany Barcelona, November 07, 2007 Dust Effects Role of dust in global climate forcing
WEATHER AND CLIMATE WHY DOES IT MATTER?
WEATHER AND CLIMATE Rising global average temperature is associated with widespread changes in weather patterns. Scientific studies indicate that extreme weather events such as heat waves and large storms
DESCRIBING DESERT, TAIGA, AND TUNDRA BIOMES
Lesson B5 1 DESCRIBING DESERT, TAIGA, AND TUNDRA BIOMES Unit B. Science and Technology in Wildlife Management Problem Area 5. Desert, Taiga, and Tundra Biomes National Academic Standard. NS.9-12.1 Science
5 day Training on Climate Change and Adaptation
Training Programme 5 day Training on and Adaptation Developed by: Bangladesh Centre for Advanced Studies (BCAS) [A comprehensive training module along with guideline for trainers aiming to enhance capacity
How Do Oceans Affect Weather and Climate?
How Do Oceans Affect Weather and Climate? In Learning Set 2, you explored how water heats up more slowly than land and also cools off more slowly than land. Weather is caused by events in the atmosphere.
Annex eleven: Climate Change Scenarios
Annex eleven: Climate Change Scenarios 1. SCENARIOS OF CLIMATE CHANGE SECOND NATIONAL COMMUNICATION Rainfall: Maps 9 (a, b and c) show the relationship between present and future status. The red colour
Chapter 3: Climate and Climate Change Answers
Chapter 3: Climate and Climate Change Answers Section A: Climate 1. (a) Explain what each of the following means: (4 x 1 mark) (i) climate the average weather of an area over a 25 30 year period (ii) maritime
7613-1 - Page 1. Weather Unit Exam Pre-Test Questions
Weather Unit Exam Pre-Test Questions 7613-1 - Page 1 Name: 1) Equal quantities of water are placed in four uncovered containers with different shapes and left on a table at room temperature. From which
VENTILATIVE COOLING EBC ANNEX 62 PER HEISELBERG DEPARTMENT OF CIVIL ENGINEERING
VENTILATIVE COOLING EBC ANNEX 62 PER HEISELBERG DEFINITION OF VENTILATIVE COOLING VENTILATIVE COOLING IS APPLICATION (DISTRIBUTION IN TIME AND SPACE) OF VENTILATION AIR FLOW TO REDUCE COOLING LOADS IN
Impacts of a future city master plan on on thermal and wind environments in Vinh city, Vietnam
Impacts of a future city master plan on on thermal and wind environments in Vinh city, Vietnam Satoru Iizuka, Nagoya University, Japan Tatsunori Ito, Nagoya University, Japan Masato Miyata, Mitsubishi
Managing Extreme Weather at Transport for London. ARCC Assembly - 12 June 2014 Helen Woolston, Transport for London Sustainability Coordinator
Managing Extreme Weather at Transport for London ARCC Assembly - 12 June 2014 Helen Woolston, Transport for London Sustainability Coordinator Slide list (wont show) Long Term Climate Change 1. What TfL
List 10 different words to describe the weather in the box, below.
Weather and Climate Lesson 1 Web Quest: What is the Weather? List 10 different words to describe the weather in the box, below. How do we measure the weather? Use this web link to help you: http://www.bbc.co.uk/weather/weatherwise/activities/weatherstation/
The Climate of Oregon Climate Zone 2 Willamette Valley
/05 E-55 No. ci oi Unbound issue e2_, Does not circulate Special Report 914 May 1993 The Climate of Oregon Climate Zone 2 Property of OREGON STATE UNIVERSITY Library Serials Corvallis, OR 97331-4503 Agricultural
Climate change and heating/cooling degree days in Freiburg
339 Climate change and heating/cooling degree days in Freiburg Finn Thomsen, Andreas Matzatrakis Meteorological Institute, Albert-Ludwigs-University of Freiburg, Germany Abstract The discussion of climate
Energy efficient home design
Energy efficient home design GUIDELINES How an energy efficient home can help you live in comfort and save money An energy efficient home is designed to provide shade and allow cooling breezes to enter
Earth Sciences -- Grades 9, 10, 11, and 12. California State Science Content Standards. Mobile Climate Science Labs
Earth Sciences -- Grades 9, 10, 11, and 12 California State Science Content Standards Covered in: Hands-on science labs, demonstrations, & activities. Investigation and Experimentation. Lesson Plans. Presented
The State of the Climate And Extreme Weather. Deke Arndt NOAA s National Climatic Data Center
The State of the Climate And Extreme Weather Deke Arndt June Feb 2013 2011 1 The world s largest archive of weather and climate data NCDC is located in Asheville, North Carolina A place of active retirement
Deserts, Wind Erosion and Deposition
Deserts, Wind Erosion and Deposition By definition, a desert has less than 10 in (25 cm) of precipitation per year. Deserts occur at 30 o and 60 o in regions of descending air. Deserts can be hot or cold.
James Hansen, Reto Ruedy, Makiko Sato, Ken Lo
If It s That Warm, How Come It s So Damned Cold? James Hansen, Reto Ruedy, Makiko Sato, Ken Lo The past year, 2009, tied as the second warmest year in the 130 years of global instrumental temperature records,
Climate Futures Evaluation and Synthesis Tool
Climate Futures Evaluation and Synthesis Tool September 2015 Alexander Epstein, Ben Rasmussen, and Chris Cutler The National Transportation Systems Center Advancing transportation innovation for the public
Tropical Rainforest. Abiotic Factors Amount of Water, Sunlight, Soil, Precipitation
World Biomes A biome is an area of land that shares similar temperatures and precipitation. The observation of the temperature and precipitation over a period time make up a biome s climate. Each biome
Assessing energy equivalence using the peer review process. Peer review guideline
Assessing energy equivalence using the peer review process Peer review guideline October 2010 Contents 1. Background... 2 Application...3 Assumptions...3 Legislation...3 2. What is peer review?... 3 3.
LATITUDES INTERNATIONAL DESIGN CHALLENGE 2015-16
LATITUDES INTERNATIONAL DESIGN CHALLENGE 2015-16 Design Challenge Resilient working environments: carving the city for small businesses in London Submitted by: University of Westminster MSc Architecture
Natural Disasters and Climate Change in the Alps
Natural Disasters and Climate Change in the Alps Gerhard Berz University of Munich Over the last few decades, the global community has been confronted with a drastic increase in the scope and frequency
Lab Activity on the Causes of the Seasons
Lab Activity on the Causes of the Seasons 2002 Ann Bykerk-Kauffman, Dept. of Geological and Environmental Sciences, California State University, Chico * Objectives When you have completed this lab you
Central Oregon Climate and how it relates to gardening
Central Oregon Climate and how it relates to gardening Garden Note #1 Amy Jo Detweiler Horticulture Faculty Rev. July 2009 Behind the beauty of the High Desert landscape lies many factors that create challenges
The Oceans Role in Climate
The Oceans Role in Climate Martin H. Visbeck A Numerical Portrait of the Oceans The oceans of the world cover nearly seventy percent of its surface. The largest is the Pacific, which contains fifty percent
Global Seasonal Phase Lag between Solar Heating and Surface Temperature
Global Seasonal Phase Lag between Solar Heating and Surface Temperature Summer REU Program Professor Tom Witten By Abstract There is a seasonal phase lag between solar heating from the sun and the surface
AIR TEMPERATURE IN THE CANADIAN ARCTIC IN THE MID NINETEENTH CENTURY BASED ON DATA FROM EXPEDITIONS
PRACE GEOGRAFICZNE, zeszyt 107 Instytut Geografii UJ Kraków 2000 Rajmund Przybylak AIR TEMPERATURE IN THE CANADIAN ARCTIC IN THE MID NINETEENTH CENTURY BASED ON DATA FROM EXPEDITIONS Abstract: The paper
Water & Climate Review
Water & Climate Review 1. The cross section below shows the direction of air flowing over a mountain. Points A and B are at the same elevation on opposite sides of the mountain. 4. The graph below shows
CHAPTER 5 PHOTOVOLTAIC SYSTEM DESIGN
CHAPTER 5 PHOTOVOLTAIC SYSTEM DESIGN 5.1 Introduction So far in the development of this research, the focus has been to estimate the available insolation at a particular location on the earth s surface
Climate Change. Lauma M. Jurkevics - DWR, Southern Region Senior Environmental Scientist
Climate Change A n o t h e r F a c t o r i n M a n a g i n g S o u t h e r n C a l i f o r n i a s W a t e r R e s o u r c e s Lauma M. Jurkevics - DWR, Southern Region Senior Environmental Scientist USEPA-Region
Empirical study of the temporal variation of a tropical surface temperature on hourly time integration
Global Advanced Research Journal of Physical and Applied Sciences Vol. 4 (1) pp. 051-056, September, 2015 Available online http://www.garj.org/garjpas/index.htm Copyright 2015 Global Advanced Research
Ok, so if the Earth weren't tilted, we'd have a picture like the one shown below: 12 hours of daylight at all latitudes more insolation in the
Ok, so if the Earth weren't tilted, we'd have a picture like the one shown below: 12 hours of daylight at all latitudes more insolation in the tropics, less at higher latitudes Ok, so if the Earth weren't
CHAPTER 3. The sun and the seasons. Locating the position of the sun
zenith 90 summer solstice 75 equinox 52 winter solstice 29 altitude angles observer Figure 3.1: Solar noon altitude angles for Melbourne SOUTH winter midday shadow WEST summer midday shadow summer EAST