What is the IPCC? Intergovernmental Panel on Climate Change

Size: px
Start display at page:

Download "What is the IPCC? Intergovernmental Panel on Climate Change"

Transcription

1 IPCC WG1 FAQ

2 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 Environment Programme (UNEP). Its constituency is made of : The governments: the IPCC is open to all member countries of WMO and UNEP. Governments participate in plenary Sessions of the IPCC where main decisions about the IPCC work programm are taken and reports are accepted, adopted and approved. They also participate the review of IPCC Reports. The scientists: hundreds of scientists all over the world contribute to the work of the IPCC as authors, contributors and reviewers. Its role is to assess on a comprehensive, objective, open and transparent basis the latest scientific, technical and socio-economic literature produced worldwide relevant to the understanding of the risk of human-induced climate change, its observed and projected impacts and options for adaptation and mitigation.

3 Human Activities vs. Natural Influences

4

5 How are Temperatures on Earth Changing? Warming from the 1920s to 1940s = (.35 o C) 1970s to present = (.55 o C) Increased rate of warming over the previous 25 years 11 of 12 warmest years on record in the past 12 years Warming greater over land Warming slightly greater during winter Cooler areas: Northern North Atlantic near southern Greenland

6 How are Temperatures on Earth Changing? Most warming in middle and lower latitudes, particularly tropical oceans Since 1950s, decrease in # of cold days and increase in # of warm days Length of frost-free season increased in most mid- and high-latitude regions of both hemispheres NH earlier start to spring

7

8 How is Precipitation Changing? Significantly wetter in eastern North and South America, northern Europe, and northern and central Asia Drier in Sahel, southern Africa, Mediterranean, and southern Asia More precip now falls as rain instead of snow Increases in heavy precip events has occurred even in drier places Increases in both droughts and floods

9 Palmer Drought Severity Index (Measure of soil moisture)

10 How is Precipitation Changing? Soil moisture acts as air conditioner. Wetter areas (eastern NA and SA) show a smaller temperature increase Water vapor has increased globally by 5% over the oceans which has increased precipitation intensity and risk of heavy rain and snow events Therefore, warmer climate increases risk of both drought where it is not raining and floods- where it is raining More rain less snow equals less snow pack which reduces summer water availability when it is most needed.

11 Change in Extreme Events? Since 1950 the number of heat waves has increased In the last 50 years, significant decrease in cold nights In the last 50 years, significant increase in warm nights Since 1970, 75% increase in Category 4 and 5 hurricanes

12

13 Amount of Snow and Ice Decreasing? YES. Observations show a globalscale decline of snow and ice over many years, especially since Mountain glaciers are shrinking Snow is retreating earlier in spring Sea ice is shrinking Permafrost reductions are widespread Snow cover has declined by about 2% per decade since 1966 Glacier, ice cap, ice sheet melt to sea level rise is estimated to be mm/yr between 1993 and 2003

14

15 Is Sea Level Rising? YES. There is strong evidence that sea level gradually rose in the 20 th century and is currently rising at an increased rate, after a period of little change between AD 0 and AD 1900 Sea level is predicted to rise at an even greater rate in this century 20 th century estimates of 1.7 mm per year

16

17 Is the Current Climate Change Historically Unusual? Concentration of CO 2 has reached a record high relative to more than the past 500,000 years and has done so at an exceptionally fast rate Most of the warming in the past 50 years is attributable to human activities CO 2 concentrations are known accurately for the past 650,000 years. During that time, they varied between 180 ppm and 300 ppm. Now CO 2 is 379 ppm which took about 100 years to increase For comparison, it took over 5,000 years for an 80 ppm rise after the last ice age. Higher values than today have only occurred over many millions of years

18 Is the Current Climate Change Historically Unusual? While there are differences between climate reconstructions, all published reconstructions find that temperatures were warm during medieval times, cooled to low values in the 17 th, 18 th, and19th centuries, and warmed rapidly after that The current RATE of global warming is much more rapid and very unusual in the context of past changes Although large climate changes have occurred in the past, there is no evidence that they took place at a faster rate than the present warming If projections of a 5 o C warming in this century are realized, Earth will have experienced the same amount of global warming as it did at the end of the last ice age There is no evidence that this rate is matched to a comparable global temperature increase over the last 50 million years!

19 Are the Increases in Greenhouse Gases Caused by Humans? YES. In fact, the full extent of the increases is not seen because atmospheric concentrations only account for 55% of the human activity The rest is absorbed by plants and the oceans The relative amount of 13 C in air has been declining which means that the added C is from plants and fossil fuels made from prehistoric plants/animals Between 1960 and 1999 CH 4 concentrations grew at a rate of 6 times faster than over any previous 40 year period in the last 2,000 years Between 1960 and 1999, N 2 O concentrations grew at least twice as fast than over any other 40 year period in the previous 2000 years The 38% increase of tropospheric ozone since the pre-industrial era is human-caused. It is very likely that the increase in combined radiative forcing from CO 2, CH4, and N 2 O was at least 6 times faster between 1960 and 1999 than over any 40 year period in the last 2,000 years

20 How Reliable are Climate Models? VERY. Models can reproduce past and present climate Models have consistently provided a robust and unambiguous picture of significant climate warming in response to increasing greenhouse gases Despite some uncertainties (clouds, aerosols, etc.) models are unanimous in their predictions of substantial climate warming under greenhouse gas increases

21 How Reliable are Climate Models?

22 Could the Warming be Natural? Very unlikely that the 20 th century warming can be explained by natural causes Climate records indicate that the 2 nd half of the 20 th century was likely the warmest 50- year period in the NH in the last 1,300 years Models fail to reproduce the observed climate when human activities are removed When human activities are added, models accurately reflect past and present climate changes The human influence on climate very likely dominates over all other causes of climate change during the past 50 years

23 Could the Warming be Natural? No.

24 More Extreme Events? YES. Already increase in frequency and intensity of heat waves and heavy precip events Fewer frost days Increased growing season Fewer cold air outbreaks More summer dryness, winter wetness Intense heavy downpours but also longer dry periods Wet areas will get wetter, dry areas drier More runoff means more warm season floods More intense tropical storms, greater wind speeds and rainfall

25 Day After Tomorrow? Not considered likely in the 21 st century However, such changes may be more likely with time if climate change continues unabated Even if the ocean circulation shut down the relative warming from increased greenhouse gases would overwhelm the cooling due to a colder Atlantic Ocean No climate model predicts Day After Tomorrow even under worst-case scenarios

26 What if Greenhouse Gases were Reduced? Some concentrations decline almost immediately while others still increase for centuries Ex. more than 50% of CO 2 is removed by oceans, 20% remains for thousands of years Therefore, CO 2 concentrations will continue to increase in the long term even if they are reduced today Only a complete shut-off of CO 2 emissions would result in a long-term stabilization at a constant level Cutting CO 2 emissions by 50% today will only stabilize the levels for the next 10 years

27 Work Cited IPCC, 2007: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change [Solomon, S., D. Qin, M. Manning, Z. Chen, M. Marquis, K.B. Averyt, M.Tignor and H.L. Miller (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA.

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

Global warming is unequivocal: The 2007 IPCC Assessment

Global warming is unequivocal: The 2007 IPCC Assessment Global warming is unequivocal: The 2007 IPCC Assessment Kevin E. Trenberth * March 2, 2007 * Any opinions, findings, conclusions, or recommendations expressed in this publication are those of the author

More information

3. Climate Change. 3.1 Observations 3.2 Theory of Climate Change 3.3 Climate Change Prediction 3.4 The IPCC Process

3. Climate Change. 3.1 Observations 3.2 Theory of Climate Change 3.3 Climate Change Prediction 3.4 The IPCC Process 3. Climate Change 3.1 Observations 3.2 Theory of Climate Change 3.3 Climate Change Prediction 3.4 The IPCC Process 3.1 Observations Need to consider: Instrumental climate record of the last century or

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

Chapter 2. Changes in Sea Level Melting Cryosphere Atmospheric Changes Summary IPCC (2013)

Chapter 2. Changes in Sea Level Melting Cryosphere Atmospheric Changes Summary IPCC (2013) IPCC (2013) Ice is melting faster (sea ice, glaciers, ice sheets, snow) Sea level is rising More ocean heat content More intense rainfall More severe drought Fewer frosts More heat waves Spring is arriving

More information

Chapter outline. Reference 12/13/2016

Chapter outline. Reference 12/13/2016 Chapter 2. observation CC EST 5103 Climate Change Science Rezaul Karim Environmental Science & Technology Jessore University of science & Technology Chapter outline Temperature in the instrumental record

More information

Extremes of Weather and the Latest Climate Change Science. Prof. Richard Allan, Department of Meteorology University of Reading

Extremes of Weather and the Latest Climate Change Science. Prof. Richard Allan, Department of Meteorology University of Reading Extremes of Weather and the Latest Climate Change Science Prof. Richard Allan, Department of Meteorology University of Reading Extreme weather climate change Recent extreme weather focusses debate on climate

More information

Global Climate Change and the Implications for Oklahoma. Gary McManus Associate State Climatologist Oklahoma Climatological Survey

Global Climate Change and the Implications for Oklahoma. Gary McManus Associate State Climatologist Oklahoma Climatological Survey Global Climate Change and the Implications for Oklahoma Gary McManus Associate State Climatologist Oklahoma Climatological Survey OCS LEGISLATIVE MANDATES Conduct and report on studies of climate and weather

More information

Climate Variability and Change Past, Present and Future An Overview

Climate Variability and Change Past, Present and Future An Overview Climate Variability and Change Past, Present and Future An Overview Dr Jim Salinger National Institute of Water and Atmospheric Research Auckland, New Zealand INTERNATIONAL WORKSHOP ON REDUCING VULNERABILITY

More information

What is Climate? Climate Change Evidence & Causes. Is the Climate Changing? Is the Climate Changing? Is the Climate Changing? Is the Climate Changing?

What is Climate? Climate Change Evidence & Causes. Is the Climate Changing? Is the Climate Changing? Is the Climate Changing? Is the Climate Changing? What is Climate? 1 Climate Change Evidence & Causes Refers to the average environmental conditions (i.e. temperature, precipitation, extreme events) in a given location over many years Climate is what

More information

THE CANADIAN CENTRE FOR CLIMATE MODELLING AND ANALYSIS

THE CANADIAN CENTRE FOR CLIMATE MODELLING AND ANALYSIS THE CANADIAN CENTRE FOR CLIMATE MODELLING AND ANALYSIS As Canada s climate changes, and weather patterns shift, Canadian climate models provide guidance in an uncertain future. CANADA S CLIMATE IS CHANGING

More information

Global warming and Extremes of Weather. Prof. Richard Allan, Department of Meteorology University of Reading

Global warming and Extremes of Weather. Prof. Richard Allan, Department of Meteorology University of Reading Global warming and Extremes of Weather Prof. Richard Allan, Department of Meteorology University of Reading Extreme weather climate change Recent extreme weather focusses debate on climate change Can we

More information

Historical and Projected National and Regional Climate Trends

Historical and Projected National and Regional Climate Trends Climate Change Trends for Planning at Sand Creek Massacre National Historic Site Prepared by Nicholas Fisichelli, NPS Climate Change Response Program April 18, 2013 Climate change and National Parks Climate

More information

Global Climate Change and the Implications for Oklahoma. Gary McManus Associate State Climatologist Oklahoma Climatological Survey

Global Climate Change and the Implications for Oklahoma. Gary McManus Associate State Climatologist Oklahoma Climatological Survey Global Climate Change and the Implications for Oklahoma Gary McManus Associate State Climatologist Oklahoma Climatological Survey Our previous stance on global warming Why the anxiety? Extreme Viewpoints!

More information

Lecture 28: Observed Climate Variability and Change

Lecture 28: Observed Climate Variability and Change Lecture 28: Observed Climate Variability and Change 1. Introduction This chapter focuses on 6 questions - Has the climate warmed? Has the climate become wetter? Are the atmosphere/ocean circulations changing?

More information

Climate Change. Unit 3

Climate Change. Unit 3 Climate Change Unit 3 Aims Is global warming a recent short term phenomenon or should it be seen as part of long term climate change? What evidence is there of long-, medium-, and short- term climate change?

More information

Global Warming: The known, the unknown, and the unknowable

Global Warming: The known, the unknown, and the unknowable Global Warming: The known, the unknown, and the unknowable Barry A. Klinger Jagadish Shukla George Mason University (GMU) Institute of Global Environment and Society (IGES) January, 2008, George Mason

More information

Extremes Events in Climate Change Projections Jana Sillmann

Extremes Events in Climate Change Projections Jana Sillmann Extremes Events in Climate Change Projections Jana Sillmann Max Planck Institute for Meteorology International Max Planck Research School on Earth System Modeling Temperature distribution IPCC (2001) Outline

More information

Introduction to Global Warming

Introduction to Global Warming Introduction to Global Warming Cryosphere (including sea level) and its modelling Ralf GREVE Institute of Low Temperature Science Hokkaido University Sapporo, 2010.09.14 http://wwwice.lowtem.hokudai.ac.jp/~greve/

More information

Weather and Climate Change

Weather and Climate Change Weather and Climate Change What if the environmental lapse rate falls between the moist and dry adiabatic lapse rates? The atmosphere is unstable for saturated air parcels but stable for unsaturated air

More information

Introduction to Climate Change

Introduction to Climate Change Ch 19 Climate Change Introduction to Climate Change Throughout time, the earth's climate has always been changing produced ice ages Hence, climate variations have been noted in the past what physical processes

More information

Chapter Introduction. Earth. Change. Chapter Wrap-Up

Chapter Introduction. Earth. Change. Chapter Wrap-Up Chapter Introduction Lesson 1 Lesson 2 Lesson 3 Climates of Earth Chapter Wrap-Up Climate Cycles Recent Climate Change What is climate and how does it impact life on Earth? What do you think? Before you

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

Future Climate Change

Future Climate Change Future Climate Change How do you know whether to trust a prediction about the future? All predictions are based on global circulation models (GCMs, AOGCMs) - model accuracy is verified by its ability to

More information

Observed changes in climate and their effects

Observed changes in climate and their effects 1 1.1 Observations of climate change Since the TAR, progress in understanding how climate is changing in space and time has been gained through improvements and extensions of numerous datasets and data

More information

Observed and Projected Climate Change. David R. Easterling, Ph.D. NOAA/National Climatic Data Center. Asheville, NC

Observed and Projected Climate Change. David R. Easterling, Ph.D. NOAA/National Climatic Data Center. Asheville, NC Observed and Projected Climate Change David R. Easterling, Ph.D NOAA/National Climatic Data Center Asheville, NC Introduction One of the most vigorously debated topics on Earth is the issue of climate

More information

Global Ocean Heat Content (0-700m) Other signs of (global) warming. Global Sea Level Rise. Change in upper ocean temperature ( )

Global Ocean Heat Content (0-700m) Other signs of (global) warming. Global Sea Level Rise. Change in upper ocean temperature ( ) Global Ocean Heat Content (0-700m) Change in upper ocean temperature (1955-2003) 0.25C 0.50C Solid lines are three independent estimates (95% confidence interval in grey) IPCC 2007 Fig TS.16 Trends in

More information

Current and future climate of the Cook Islands. Pacific-Australia Climate Change Science and Adaptation Planning Program

Current and future climate of the Cook Islands. Pacific-Australia Climate Change Science and Adaptation Planning Program Pacific-Australia Climate Change Science and Adaptation Planning Program Penrhyn Pukapuka Nassau Suwarrow Rakahanga Manihiki N o r t h e r n C o o k I s l a nds S o u t h e Palmerston r n C o o k I s l

More information

CLIMATE. SECTION 14.1 Defining Climate

CLIMATE. SECTION 14.1 Defining Climate Date Period Name CLIMATE SECTION.1 Defining Climate In your textbook, read about climate and different types of climate data. Put a check ( ) next to the types of data that describe climate. 1. annual

More information

Activity 2.2: Recognizing Change (Observation vs. Inference)

Activity 2.2: Recognizing Change (Observation vs. Inference) Activity 2.2: Recognizing Change (Observation vs. Inference) Teacher Notes: Evidence for Climate Change PowerPoint Slide 1 Slide 2 Introduction Image 1 (Namib Desert, Namibia) The sun is on the horizon

More information

Climate. What is climate? STUDY GUIDE FOR CONTENT MASTERY. Name Class Date

Climate. What is climate? STUDY GUIDE FOR CONTENT MASTERY. Name Class Date Climate SECTION 14.1 What is climate? In your textbook, read about climate and different types of climate data. Put a check ( ) next to the types of data that describe climate. 1. annual wind speed 4.

More information

IMPACTS OF A WARMING ARCTIC

IMPACTS OF A WARMING ARCTIC The Earth s Greenhouse Effect Most of the heat energy emitted from the surface is absorbed by greenhouse gases which radiate heat back down to warm the lower atmosphere and the surface. Increasing the

More information

Climate.tgt, Version: 1 1

Climate.tgt, Version: 1 1 Name: Key Concepts Choose the letter of the best answer. (5 points each) 1. 2. 3. 4. 5. 6. 7. 8. 9. 10. Date: A city located in the middle of North America experiences extreme temperature changes during

More information

6. What has been the most effective erosive agent in the climate system? a. Water b. Ice c. Wind

6. What has been the most effective erosive agent in the climate system? a. Water b. Ice c. Wind Multiple Choice. 1. Heinrich Events a. Show increased abundance of warm-water species of planktic foraminifera b. Show greater intensity since the last deglaciation c. Show increased accumulation of ice-rafted

More information

Climate in the Future AOSC 200 Tim Canty. Increase in temperature is correlated with increase in GHGs (and population)

Climate in the Future AOSC 200 Tim Canty. Increase in temperature is correlated with increase in GHGs (and population) Climate in the Future AOSC 200 Tim Canty Class Web Site: http://www.atmos.umd.edu/~tcanty/aosc200 Topics for today: Evidence of a changing climate Possible issues associated with a changing climate Lecture

More information

Weather Atmospheric condition in one place during a limited period of time Climate Weather patterns that an area typically experiences over a long

Weather Atmospheric condition in one place during a limited period of time Climate Weather patterns that an area typically experiences over a long Weather Atmospheric condition in one place during a limited period of time Climate Weather patterns that an area typically experiences over a long period of time Many factors influence weather & climate

More information

4 Changes in Climate. TAKE A LOOK 2. Explain Why is more land exposed during glacial periods than at other times?

4 Changes in Climate. TAKE A LOOK 2. Explain Why is more land exposed during glacial periods than at other times? Name Class CHAPTER 3 Date Climate 4 Changes in Climate SECTION National Science Education Standards BEFORE YOU READ After you read this section, you should be able to answer these questions: ES 1k, 2a

More information

Table of Contents. Chapter: Atmosphere. Section 1: Earth's Atmosphere. Section 2: Energy Transfer in the Atmosphere. Section 3: Air Movement

Table of Contents. Chapter: Atmosphere. Section 1: Earth's Atmosphere. Section 2: Energy Transfer in the Atmosphere. Section 3: Air Movement Table of Contents Chapter: Atmosphere Section 1: Earth's Atmosphere Section 2: Energy Transfer in the Atmosphere Section 3: Air Movement Table of Contents Chapter 4: Atmosphere Section 1: Earth's Atmosphere

More information

ATM S 111 Global Warming Exam Review. Jennifer Fletcher Day 31, August 3, 2010

ATM S 111 Global Warming Exam Review. Jennifer Fletcher Day 31, August 3, 2010 ATM S 111 Global Warming Exam Review Jennifer Fletcher Day 31, August 3, 2010 Earth gets most of its energy from the sun. Solar Radiation Solar radiation is mostly in visible, near infrared, and near UV

More information

Weather Atmospheric condition in one place during a limited period of time Climate Weather patterns that an area typically experiences over a long

Weather Atmospheric condition in one place during a limited period of time Climate Weather patterns that an area typically experiences over a long Weather Atmospheric condition in one place during a limited period of time Climate Weather patterns that an area typically experiences over a long period of time Many factors influence weather & climate

More information

Weather Vs. Climate. Weather Vs. Climate. Chapter 14

Weather Vs. Climate. Weather Vs. Climate. Chapter 14 Weather Vs. Climate Chapter 14 Weather: Conditions of the atmosphere at a particular time and place, for short periods of time (days). Climate: Long-term averages of weather (Averaged over 30 yrs). Weather

More information

Climate Dataset: Aitik Closure Project. November 28 th & 29 th, 2018

Climate Dataset: Aitik Closure Project. November 28 th & 29 th, 2018 1 Climate Dataset: Aitik Closure Project November 28 th & 29 th, 2018 Climate Dataset: Aitik Closure Project 2 Early in the Closure Project, consensus was reached to assemble a long-term daily climate

More information

A Tutorial on Climate Change Science: The. 4 th National Climate Assessment CLIMATE SCIENCE. Don Wuebbles

A Tutorial on Climate Change Science: The. 4 th National Climate Assessment CLIMATE SCIENCE. Don Wuebbles CLIMATE SCIENCE S P E C I A L R E P O R T A Tutorial on Climate Change Science: The Fourth National Climate Assessment Volume I 4 th National Climate Assessment Don Wuebbles Department of Atmospheric Sciences

More information

Day 1 of Global Warming. Copyright 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings

Day 1 of Global Warming. Copyright 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Day 1 of Global Warming Copyright 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings The Atmosphere Atmosphere = the thin layer (1/100 th of Earth s diameter) of gases that surrounds

More information

Projections of future climate change

Projections of future climate change Projections of future climate change Matthew Collins 1,2 and Catherine A. Senior 2 1 Centre for Global Atmospheric Modelling, Department of Meteorology, University of Reading 2 Met Office Hadley Centre,

More information

Climate Change in the Northeast

Climate Change in the Northeast Climate Change in the Northeast Dr. Alan K. Betts Atmospheric Research, Pittsford, VT 05763 akbetts@aol.com http://alanbetts.com NNECAPA Stowe, VT September 11, 2014 Outline Science of climate change Global

More information

Observed State of the Global Climate

Observed State of the Global Climate WMO Observed State of the Global Climate Jerry Lengoasa WMO June 2013 WMO Observations of Changes of the physical state of the climate ESSENTIAL CLIMATE VARIABLES OCEANIC ATMOSPHERIC TERRESTRIAL Surface

More information

B. The Observed Changes in the Climate System

B. The Observed Changes in the Climate System gases (decades to centuries), and, as a result, their concentrations respond much more quickly to changes in emissions. Volcanic activity can inject large amounts of sulphur-containing gases (primarily

More information

Ocean s Influence on Weather and Climate

Ocean s Influence on Weather and Climate Earth is often called the Blue Planet because so much of its surface (about 71%) is covered by water. Of all the water on Earth, about 96.5%, is held in the world s oceans. As you can imagine, these oceans

More information

GLOBAL WARMING AND THE GREENHOUSE EFFECT

GLOBAL WARMING AND THE GREENHOUSE EFFECT GLOBAL WARMING AND THE GREENHOUSE EFFECT Our planet temperature is warming significantly due to human activities? OR Last few years warming is part of a natural global cycle? 1998 : The warmest year on

More information

World Geography Chapter 3

World Geography Chapter 3 World Geography Chapter 3 Section 1 A. Introduction a. Weather b. Climate c. Both weather and climate are influenced by i. direct sunlight. ii. iii. iv. the features of the earth s surface. B. The Greenhouse

More information

Name Date Class. growth rings of trees, fossilized pollen, and ocean. in the northern hemisphere.

Name Date Class. growth rings of trees, fossilized pollen, and ocean. in the northern hemisphere. Lesson Outline LESSON 2 A. Long-Term Cycles 1. A(n) climate cycle takes much longer than a lifetime to complete. a. To learn about long-term climate cycles, scientists study natural records, such as growth

More information

CLIMATE READY BOSTON. Climate Projections Consensus ADAPTED FROM THE BOSTON RESEARCH ADVISORY GROUP REPORT MAY 2016

CLIMATE READY BOSTON. Climate Projections Consensus ADAPTED FROM THE BOSTON RESEARCH ADVISORY GROUP REPORT MAY 2016 CLIMATE READY BOSTON Sasaki Steering Committee Meeting, March 28 nd, 2016 Climate Projections Consensus ADAPTED FROM THE BOSTON RESEARCH ADVISORY GROUP REPORT MAY 2016 WHAT S IN STORE FOR BOSTON S CLIMATE?

More information

Northern Rockies Adaptation Partnership: Climate Projections

Northern Rockies Adaptation Partnership: Climate Projections Northern Rockies Adaptation Partnership: Climate Projections Contents Observed and Projected Climate for the NRAP Region... 2 Observed and Projected Climate for the NRAP Central Subregion... 8 Observed

More information

Today. Jovian planets. but first - a little more Climate change

Today. Jovian planets. but first - a little more Climate change Today Jovian planets but first - a little more Climate change Weather and Climate Weather is the ever-varying combination of wind, clouds, temperature, and pressure. Local complexity of weather makes it

More information

Factors That Affect Climate

Factors That Affect Climate Factors That Affect Climate Factors That Affect Climate Latitude As latitude (horizontal lines) increases, the intensity of solar energy decreases. The tropical zone is between the tropic of Cancer and

More information

Chapter 3 Packet. and causes seasons Earth tilted at 23.5 / 365 1/4 days = one year or revolution

Chapter 3 Packet. and causes seasons Earth tilted at 23.5 / 365 1/4 days = one year or revolution Name Chapter 3 Packet Sequence Section 1 Seasons and Weather : and causes seasons Earth tilted at 23.5 / 365 1/4 days = one year or revolution solstice - begins summer in N. hemisphere, longest day winter

More information

Extreme Weather and Climate Change: the big picture Alan K. Betts Atmospheric Research Pittsford, VT NESC, Saratoga, NY

Extreme Weather and Climate Change: the big picture Alan K. Betts Atmospheric Research Pittsford, VT   NESC, Saratoga, NY Extreme Weather and Climate Change: the big picture Alan K. Betts Atmospheric Research Pittsford, VT http://alanbetts.com NESC, Saratoga, NY March 10, 2018 Increases in Extreme Weather Last decade: lack

More information

Observed Climate Variability and Change: Evidence and Issues Related to Uncertainty

Observed Climate Variability and Change: Evidence and Issues Related to Uncertainty Observed Climate Variability and Change: Evidence and Issues Related to Uncertainty David R. Easterling National Climatic Data Center Asheville, North Carolina Overview Some examples of observed climate

More information

Update on Climate Science. Professor Richard Betts, Met Office

Update on Climate Science. Professor Richard Betts, Met Office Update on Climate Science Professor Richard Betts, Met Office The science of climate change Crown copyright Met Office Prof Richard Betts Head of Climate Impacts Research Crown copyright Met Office Observing

More information

2) The Changing Water Cycle

2) The Changing Water Cycle 2) The Changing Water Cycle Estimates of the current global water budget and its annual flow using observations from 2002-2008 (1000 km3 for storage and 1000 km 3 yr 1 for exchanges). Based on K.E. Trenberth,

More information

1 What Is Climate? TAKE A LOOK 2. Explain Why do areas near the equator tend to have high temperatures?

1 What Is Climate? TAKE A LOOK 2. Explain Why do areas near the equator tend to have high temperatures? CHAPTER 17 1 What Is Climate? SECTION Climate BEFORE YOU READ After you read this section, you should be able to answer these questions: What is climate? What factors affect climate? How do climates differ

More information

The Atmosphere Made up of mainly two gases: Nitrogen 78% Oxygen 21% Trace Gases 1%

The Atmosphere Made up of mainly two gases: Nitrogen 78% Oxygen 21% Trace Gases 1% The Atmosphere 18.1 The Atmosphere Made up of mainly two gases: Nitrogen 78% Oxygen 21% Trace Gases 1% Layers of the Atmosphere made made up of 5 layers: Troposphere Stratosphere Mesosphere Ionosphere

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

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

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

Environmental Science Chapter 13 Atmosphere and Climate Change Review

Environmental Science Chapter 13 Atmosphere and Climate Change Review Environmental Science Chapter 13 Atmosphere and Climate Change Review Multiple Choice Identify the choice that best completes the statement or answers the question. 1. Climate in a region is a. the long-term,

More information

1 What Is Climate? TAKE A LOOK 2. Explain Why do areas near the equator tend to have high temperatures?

1 What Is Climate? TAKE A LOOK 2. Explain Why do areas near the equator tend to have high temperatures? CHAPTER 17 1 What Is Climate? SECTION Climate BEFORE YOU READ After you read this section, you should be able to answer these questions: What is climate? What factors affect climate? How do climates differ

More information

Meteorology Practice Test

Meteorology Practice Test Meteorology Practice Test 1. Transition zones between two air masses of different densities are called what? 2. A front occurs when a cold air mass replaces a warmer one. 3. A front occurs when a warm

More information

The Failed Science of Global warming: Time to Re-consider Climate Change

The Failed Science of Global warming: Time to Re-consider Climate Change The Failed Science of Global warming: Time to Re-consider Climate Change Madhav Khandekar Expert Reviewer IPCC 2007 Climate Change IPCC vs NIPCC IPCC: Intergovernmental Panel on Climate Change; A UN Body

More information

Factors that Affect Climate

Factors that Affect Climate Factors that Affect Climate What is climate? Climate is the average weather conditions over a long period of time Includes average temperatures and precipitation, wind patterns, humidity, air pressure

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

Atmosphere - Part 2. High and Low Pressure Systems

Atmosphere - Part 2. High and Low Pressure Systems Atmosphere - Part 2 High and Low Pressure Systems High Pressure vs. Low Pressure H regions : cool air sinks, increasing the air density, thus resulting in an area of high pressure L regions: warm air rises,

More information

Australian Meteorological and Oceanographic Society (AMOS) Statement on Climate Change

Australian Meteorological and Oceanographic Society (AMOS) Statement on Climate Change Australian Meteorological and Oceanographic Society (AMOS) Statement on Climate Change This statement provides a summary of some aspects of climate change and its uncertainties, with particular focus on

More information

Climate change: How do we know?

Climate change: How do we know? Climate change: How do we know? This graph, based on the comparison of atmospheric samples contained in ice cores and more recent direct measurements, provides evidence that atmospheric CO2 has increased

More information

Climates are described by the same conditions used to describe

Climates are described by the same conditions used to describe 58 The Causes of Climate R EA 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

More information

Climate Chapter 19. Earth Science, 10e. Stan Hatfield and Ken Pinzke Southwestern Illinois College

Climate Chapter 19. Earth Science, 10e. Stan Hatfield and Ken Pinzke Southwestern Illinois College Climate Chapter 19 Earth Science, 10e Stan Hatfield and Ken Pinzke Southwestern Illinois College The climate system A. Climate is an aggregate of weather B. Involves the exchanges of energy and moisture

More information

Climate changes in Finland, but how? Jouni Räisänen Department of Physics, University of Helsinki

Climate changes in Finland, but how? Jouni Räisänen Department of Physics, University of Helsinki Climate changes in Finland, but how? Jouni Räisänen Department of Physics, University of Helsinki 19.9.2012 Outline Some basic questions and answers about climate change How are projections of climate

More information

Climate Change: Updated scientific assessment. Kevin E Trenberth NCAR. Help!

Climate Change: Updated scientific assessment. Kevin E Trenberth NCAR. Help! Climate Change: Updated scientific assessment Help! Kevin E Trenberth NCAR Running a fever: Seeing the doctor Symptoms: the planet s temperature and carbon dioxide are increasing Diagnosis: human activities

More information

What is Climate? Understanding and predicting climatic changes are the basic goals of climatology.

What is Climate? Understanding and predicting climatic changes are the basic goals of climatology. What is Climate? Understanding and predicting climatic changes are the basic goals of climatology. Climatology is the study of Earth s climate and the factors that affect past, present, and future climatic

More information

( 1 d 2 ) (Inverse Square law);

( 1 d 2 ) (Inverse Square law); ATMO 336 -- Exam 3 120 total points including take-home essay Name The following equations and relationships may prove useful. F d1 =F d2 d 2 2 ( 1 d 2 ) (Inverse Square law);! MAX = 0.29 " 104 µmk (Wien's

More information

Appendix 1: UK climate projections

Appendix 1: UK climate projections Appendix 1: UK climate projections The UK Climate Projections 2009 provide the most up-to-date estimates of how the climate may change over the next 100 years. They are an invaluable source of information

More information

May Global Warming: Recent Developments and the Outlook for the Pacific Northwest

May Global Warming: Recent Developments and the Outlook for the Pacific Northwest Global Warming: Recent Developments and the Outlook for the Pacific Northwest Pat Bartlein Department of Geography University of Oregon (bartlein@uoregon.edu) http://geography.uoregon.edu/envchange/gwhr/

More information

Climate versus Weather

Climate versus Weather Climate versus Weather What is climate? Climate is the average weather usually taken over a 30-year time period for a particular region and time period. Climate is not the same as weather, but rather,

More information

ATOC OUR CHANGING ENVIRONMENT Class 19 (Chp 6) Objectives of Today s Class: The Cryosphere [1] Components, time scales; [2] Seasonal snow

ATOC OUR CHANGING ENVIRONMENT Class 19 (Chp 6) Objectives of Today s Class: The Cryosphere [1] Components, time scales; [2] Seasonal snow ATOC 1060-002 OUR CHANGING ENVIRONMENT Class 19 (Chp 6) Objectives of Today s Class: The Cryosphere [1] Components, time scales; [2] Seasonal snow cover, permafrost, river and lake ice, ; [3]Glaciers and

More information

WEATHER. rain. thunder. The explosive sound of air as it is heated by lightning.

WEATHER. rain. thunder. The explosive sound of air as it is heated by lightning. WEATHER rain thunder The explosive sound of air as it is heated by lightning. rainbow lightning hurricane They are intense storms with swirling winds up to 150 miles per hour. tornado cold front warm front

More information

Prentice Hall EARTH SCIENCE

Prentice Hall EARTH SCIENCE Prentice Hall EARTH SCIENCE Tarbuck Lutgens Chapter 21 Climate 21.1 Factors That Affect Climate Factors That Affect Climate Latitude As latitude increases, the intensity of solar energy decreases. The

More information

Prentice Hall EARTH SCIENCE

Prentice Hall EARTH SCIENCE Prentice Hall EARTH SCIENCE Tarbuck Lutgens Chapter 21 Climate 21.1 Factors That Affect Climate Factors That Affect Climate Latitude As latitude increases, the intensity of solar energy decreases. The

More information

Factors that Affect Climate

Factors that Affect Climate Factors that Affect Climate What is climate? Climate is the average weather conditions over a long period of time Includes average temperatures and precipitation, wind patterns, humidity, air pressure

More information

CH. 3: Climate and Vegetation

CH. 3: Climate and Vegetation CH. 3: Climate and Vegetation GROUP WORK RUBRIC Score of 50 (5): Superior - 100% A 5 is superior work, and has completed all requirements of the assignments, it is in order and its presentation is almost

More information

SHAPING OUR FUTURE: THE CLIMATE CHALLENGE KS3 LESSON 1 TEACHER GUIDE HOW IS OUR CLIMATE CHANGING?

SHAPING OUR FUTURE: THE CLIMATE CHALLENGE KS3 LESSON 1 TEACHER GUIDE HOW IS OUR CLIMATE CHANGING? SHAPING OUR FUTURE: THE CLIMATE CHALLENGE KS3 LESSON 1 TEACHER GUIDE HOW IS OUR CLIMATE CHANGING? KS3 LESSON 1 TEACHER GUIDE HOW IS OUR CLIMATE CHANGING? Learning objective: To understand, through the

More information

Tropical Climates Zone

Tropical Climates Zone Tropical Climates Zone RAIN FOREST CENTRAL AFRICA, SOUTH AMERICA (AMAZON), CENTRAL AMERICA, S.E. ASIA HUMID/WARM ANNUAL RAINFALL 200 CM TYPE #1: TROPICAL DESERT N. AFRICA (SAHARA) & S.W. ASIA < 25 CM

More information

Multiple Choice Identify the choice that best completes the statement or answers the question.

Multiple Choice Identify the choice that best completes the statement or answers the question. CH.15 practice TEST Multiple Choice Identify the choice that best completes the statement or answers the question. 1) The short-term state of the atmosphere is called a) climate. c) water cycle. b) weather.

More information

Mozambique. General Climate. UNDP Climate Change Country Profiles. C. McSweeney 1, M. New 1,2 and G. Lizcano 1

Mozambique. General Climate. UNDP Climate Change Country Profiles. C. McSweeney 1, M. New 1,2 and G. Lizcano 1 UNDP Climate Change Country Profiles Mozambique 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 http://country-profiles.geog.ox.ac.uk

More information

Weather Elements (air masses, fronts & storms)

Weather Elements (air masses, fronts & storms) Weather Elements (air masses, fronts & storms) S6E4. Obtain, evaluate and communicate information about how the sun, land, and water affect climate and weather. A. Analyze and interpret data to compare

More information

Prof. Dr. Anders Levermann Junior Professor for climate modelling on long timescales, Potsdam Institute for Climate Impact Research, Potsdam, Germany

Prof. Dr. Anders Levermann Junior Professor for climate modelling on long timescales, Potsdam Institute for Climate Impact Research, Potsdam, Germany Prof. Dr. Anders Levermann Junior Professor for climate modelling on long timescales, Potsdam Institute for Climate Impact Research, Potsdam, Germany Points for discussion: The state of global climate;

More information

Summary. The Ice Ages and Global Climate

Summary. The Ice Ages and Global Climate The Ice Ages and Global Climate Summary Earth s climate system involves the atmosphere, hydrosphere, lithosphere, and biosphere. Changes affecting it operate on time scales ranging from decades to millions

More information

The Distribution of Cold Environments

The Distribution of Cold Environments The Distribution of Cold Environments Over 25% of the surface of our planet can be said to have a cold environment, but defining what we actually mean by that can be very challenging. This is because cold

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

1 What Is Climate? TAKE A LOOK 2. Explain Why do areas near the equator tend to have high temperatures?

1 What Is Climate? TAKE A LOOK 2. Explain Why do areas near the equator tend to have high temperatures? CHAPTER 3 1 What Is Climate? SECTION Climate BEFORE YOU READ After you read this section, you should be able to answer these questions: What is climate? What factors affect climate? How do climates differ

More information