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Module 1
Introduction to Climate Change Science
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Learning Objectives
1. Explain the basic concepts of climate change
science
2. Identify the anthropogenic drivers of
climate change
4. Analyze different climate change scenarios and their
implications
3. Explain observed and projected trends in the
climate
By the end of the module
participants will be able to:
Module 1: Introduction to Climate Change Science
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OVERVIEW
Section 1
Introduction to Climate Change Science
Section 2
Anthropogenic Drivers of
Climate Change
Section 3
Observed Trends and Impacts of
Climate Change
Section 4
Projected Trends and Impacts of
Climate Change
Section 5
Sources of Scientific Data
Overview
Module 1: Introduction to Climate Change Science
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Introduction to Climate
Change ScienceSection 1
Module 1: Introduction to Climate Change Science
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What Is Climate?
Weather
“What is happening in the
atmosphere at any given time”
Climate
“Average weather over longer time
frames”
Section 1: Introduction to Climate Change Science
Source: World Meteorological Organization
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Complexity of the Global Climate System
Section 1: Introduction to Climate Change Science
Source: IPCC 2007, p96. Further information: WMO
Website
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What Is the Greenhouse Effect?
Section 1: Introduction to Climate Change Science
Source: IPCC 2007. Further info: WMO Website
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NASA Video on the Greenhouse Effect
URL: http://www.youtube.com/watch?v=ZzCA60WnoMk
Section 1: Introduction to Climate Change Science
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Video: Understand how water vapor, carbon
dioxide, and other gases cause the Earth’s
greenhouse effect
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Factors Shaping the Climate –“Climate Forcings”
Section 1: Introduction to Climate Change Science
Source: NOAAA National Climatic Data Center
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Natural Climate Fluctuations –Example of El Niño and La Niña
Section 1: Introduction to Climate Change Science
Source: NOAA. Further information: WMO Website
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Climate Change and Global Warming
Global Warming
Refers to the overall warming of the planet,
based on average temperature over the
entire surface of the Earth
Climate Change
Refers to changes in climate characteristics, including temperature, humidity, rainfall, wind,
and severe weather events over long term
periods
Section 1: Introduction to Climate Change Science
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Further information: WMO Website
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Observed Change in Surface Temperature (1901–2012)
Source:
Source: IPCC 2013, p4
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Section 1: Introduction to Climate Change Science
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Tools to Predict and Project Changes in the Climate
• A climate prediction or climate “forecast” is an attempt to produce an estimate of the actual evolution of the climate in the future.
Climate Prediction
• Emissions scenarios describe future releases to the atmosphere of greenhouse gases, aerosols, and other pollutants and, along with information on land use and land cover, provide inputs to climate models.
Emissions Scenario
• A numerical representation of the climate system based on the physical, chemical and biological properties of its components, their interactions and feedback processes, and accounting for some of its known properties.
Climate Model
• A climate projection is the simulated response of the climate system to a scenario of future emission or concentration of greenhouse gases and aerosols, generally derived using climate models.
Climate Projection
Section 1: Introduction to Climate Change Science
Source: IPCC 2013 and IPCC Website. Further info: WMO Website
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Projected Change in Average Surface Temperature
Source: IPCC 2013, p20
Scenario RCP 8.5Scenario RCP 2.6
Section 1: Introduction to Climate Change Science
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Time Period: 1986-2005 to 2081-2100
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Climate Change Has an Impact on:
• Biodiversity, carbon storage, habitats, …
Ecosystems
• Agriculture, fresh water, health, …
Human systems
• Transport, buildings, lifestyle, …Urban systems
• Energy, manufacturing, natural capital industries, …
Economic systems
• Equity, migration, peace and conflict, …
Social systems
Section 1: Introduction to Climate Change Science
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Climate Change Science Allows Us to:
Understand how and why the climate is changing
Assess how humans are influencing the climate
Project how the climate may change in the future
Support policy/decision-making and changes in behaviors
Section 1: Introduction to Climate Change Science
Source: National Science Foundation
Photo Credit: Niwot Ridge lter site/John W. Marr
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Why is Climate Change Science Important?
Sound weather data and forecasts
important for:
Short-term planning
Emergency response
Climate models help to forecast long
term climate scenarios
Important input for vulnerability assessments and
adaptation planning
Fosters climate resilient development and avoids mal-
adaption
Section 1: Introduction to Climate Change Science
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History of Climate Change Science
• Argument raised that the temperature of the Earth can be augmented by the interposition of the atmosphere
1824
• Indication that CO2 and H2O can cause changes in the climate
1861
• First proposal of the idea of a man-made greenhouse effect
1895
• Proof that doubling of atmospheric CO2 concentration resulted in an increase in the mean global temperature of 2°C
1938
• Start of interdisciplinary field of carbon cycle science1950s
• The high-accuracy measurements of atmospheric CO2
concentration1958
• Other greenhouse gases widely recognised1970s
• The first World Climate Conference in Geneva1979
• Establishment of Intergovernmental Panel on Climate Change (IPCC)
1988
• The first IPCC report1990
Section 1: Introduction to Climate Change Science
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Further information: BBC
Website
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Anthropogenic Drivers of
Climate ChangeSection 2
Module 1: Introduction to Climate Change Science
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IPCC Video on the Human Influence on the Climate System
URL: http://www.youtube.com/watch?v=6yiTZm0y1YA&feature=youtu.be
Video: The video summarizes the main findings
of the 2013 IPCC Report on the physical science
basis of climate change.
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Section 2: Anthropogenic Drivers of Climate Change
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Overview of Greenhouse Gases Regulated under the Kyoto Protocol
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Greenhouse Gas Global Warming
Potential (GWP) (over
100 years)
% of Total Anthropogenic
GHG Emissions (2010)
Carbon dioxide (CO2) 1 76%
Methane (CH4) 25 16%
Nitrous oxide (N2O) 298 6%
Hydrofluorocarbons (HFCs) 124-14,800 < 2%
Perfluorocarbons (PFCs) 7,390-12,200 < 2%
Sulphur hexafluoride (SF6) 22,800 < 2%
Nitrogen trifluoride (NF3) 17,200 < 2%
Source: Reproduced from IPCC 2007 and UNEP 2012
Section 2: Anthropogenic Drivers of Climate Change
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Important Greenhouse Gases: Carbon Dioxide (CO2)
Most important greenhouse gas
(contributes ~64% to total radiative
forcing by long-lived GHGs)
Half of CO2 emitted by human activities
is being absorbed in the biosphere and
in the oceans
Rest remains in the atmosphere for
hundreds to thousands of years
Source: WMO 2013
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Section 2: Anthropogenic Drivers of Climate Change
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CO2 Concentration in the Atmosphere and Annual Growth Rates
Source: WMO 2013
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Section 2: Anthropogenic Drivers of Climate Change
Since 1750 CO2 concentration in the atmosphere has increased by 40%.
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Important Greenhouse Gases: Methane (CH4)
Second most significant greenhouse
gas (contributes ~18% to total
radiative forcing by long-lived
GHGs)
Approximately 40% of methane is
emitted into the atmosphere by
natural sources
About 60% comes from human
activities
Stays in the atmosphere for
approximately 12 years
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Section 2: Anthropogenic Drivers of Climate Change
Source: IPCC 2007 and WMO 2013
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CH4 Concentration in the Atmosphere and Annual Growth Rates25
Section 2: Anthropogenic Drivers of Climate Change
Source: WMO 2013
Since 1750 CH4 concentration in the atmosphere has increased by 150%.
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In Focus: The Carbon Cycle
Source: UNEP
Section 2: Anthropogenic Drivers of Climate Change
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Important Greenhouse Gases: Nitrous Oxide (N2O)
The third most significant
greenhouse gas (contributes ~6% to
total radiative forcing by long-lived
GHGs)
Stays in the atmosphere for
approximately 114 years
Nitrous oxide is emitted into the
atmosphere from both natural (about
60%) and anthropogenic sources
(approximately 40%)
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Section 2: Anthropogenic Drivers of Climate Change
Source: IPCC 2007 and WMO 2013
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N2O Concentration in the Atmosphere and Annual Growth Rates28
Section 2: Anthropogenic Drivers of Climate Change
Source: WMO 2013
Since 1750 N2O concentration in the atmosphere has increased by 20%.
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Important Greenhouse Gases: Fluorinated Gases
Global warming effect up to 23,000
times greater than carbon dioxide
Stay in the atmosphere up to 50,000
years
Three main groups:
hydrofluorocarbons (HFCs),
perfluorocarbons (PFCs), and sulfur
hexafluoride (SF6)
Mainly developed as substitutes for
ozone-depleting substances
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Section 2: Anthropogenic Drivers of Climate Change
Source: IPCC 2007. Further info
EPA, EC
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Greenhouse Gases Controlled by the Montreal Protocol
Montreal Protocol aimed to
phase out substances that
deplete the ozone layer
Substances regulated under the
Montreal Protocol are also
powerful greenhouse gases
For example,
chlorofluorocarbons (CFCs)
contribute ~12% to radiative
forcing by long-lived GHGs
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Section 2: Anthropogenic Drivers of Climate Change
Source: IPCC 2007 and WMO 2013. Further info: NOAA
Website
Source: EPA
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Concentration of SF6 and Halocarbons in the Atmosphere
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Section 2: Anthropogenic Drivers of Climate Change
Source: WMO 2013
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It is extremely likely that more than 50%
of the warming since 1951 is due to
the increase in greenhouse gases
and other anthropogenic
forcings together.
Human Influence on the Climate System
Source: IPCC 2013. Further info: WMO website
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Section 2: Anthropogenic Drivers of Climate Change
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Observed Trends and
Impacts of Climate ChangeSection 3
Module 1: Introduction to Climate Change Science
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Observed Surface Temperature Anomaly (1850-2012)
Source: IPCC 2013, p4
Section 3: Observed Trends and Impacts of Climate Change
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Globally averaged land and ocean surface temperature
Each of the last three decades has been successively
warmer at the Earth’s surface than
any preceding decade since 1850.
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Observed Change in Annual Precipitation Over Land
Source: IPCC 2013, p6
Section 3: Observed Trends and Impacts of Climate
Change
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Observed Ocean Warming (1950-2010)
Section 3: Observed Trends and Impacts of Climate
Change
Source: IPCC 2013, p8
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More than 60% of the net energy increase in the
climate system is stored in the upper ocean (period 1971-
2010).
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Observed Ocean Acidification
Section 3: Observed Trends and Impacts of Climate
Change
Source: IPCC 2013, p10
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Observed Sea Level Rise (1900 to 2010)
Section 3: Observed Trends and Impacts of Climate
Change
Source: IPCC 2013, p8
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Over the period 1901 to 2010,
global mean sea level rose by
0.19m.
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Observed Decrease in Arctic Sea Ice Extent (1900-2010)
Section 3: Observed Trends and Impacts of Climate
Change
Source: IPCC 2013, p8
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Observed Changes in Physical and Biological Systems
Section 3: Observed Trends and Impacts of Climate
Change
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Source: UNEP 2009, p13
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In Focus: Is Climate Change to Blame for Extreme Weather Events?
Source: UNEP
2009, p12.
Further info:
WMO Website
Section 3: Observed Trends and Impacts of Climate
Change
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Year
Nu
mbe
r of
Even
ts
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Projected Trends and
Impacts of Climate ChangeSection 4
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In Focus: Representative Concentration Pathways (RCPs)
Section 4: Projected Trends and Impacts of Climate
Change
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Set of four new scenarios defined by the scientific
community for the Fifth IPCC Assessment Report.
Four RCPs include:
one mitigation scenario leading to a very low forcing
level (RCP2.6),
two stabilization scenarios (RCP4.5 and RCP6), and
one scenario with very high greenhouse gas
emissions (RCP8.5).
RCPs represent a range of 21st century climate
policies.
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Global surface temperature change for the end of the 21st century is likely to reach 4°C if no action is
taken.
Projected Change in Average Surface Temperature
So
urc
e: IP
CC
20
13, p
19
Section 4: Projected Trends and Impacts of Climate
Change
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Projected Change in Average Precipitation
Source: IPCC 2013, p20
Scenario RCP 8.5Scenario RCP 2.6
Section 4: Projected Trends and Impacts of Climate
Change
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Time Period: 1986-2005 to 2081-2100
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Temperature and Precipitation Projections for the 21st Century
URL: http://www.youtube.com/watch?v=bFqO3_2dYxA
Video: This NASA video shows how temperature and precipitation patterns could change throughout the 21st century.
Section 4: Projected Trends and Impacts of Climate Change
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Projected Change in Ocean Surface pH
Source: IPCC 2013, p20
Scenario RCP 8.5Scenario RCP 2.6
Section 4: Projected Trends and Impacts of Climate
Change
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Time Period: 1986-2005 to 2081-2100
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Projected Sea Level Rise
Source: IPCC 2013, p24
Section 4: Projected Trends and Impacts of Climate
Change
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Global mean sea level will continue to
rise during the 21st century.
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Projected Northern Hemisphere September Sea Ice Extent
Source: IPCC 2013, p20
Scenario RCP 8.5Scenario RCP 2.6
Section 4: Projected Trends and Impacts of Climate
Change
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Average 2081-2100
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Projected Impacts of Climate Changein Africa
Source: UNEP 2009, p32
Section 4: Projected Trends and Impacts of Climate Change
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Projected Impacts of Climate Changein Asia
Section 4: Projected Trends and Impacts of Climate
Change
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Source: UNEP
2009, p34
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Projected Impacts of Climate Change in Latin America
Section 4: Projected Trends and Impacts of Climate Change
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Source: UNEP
2009, p37
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Projected Impacts of Climate Change on Small Islands
Sea level rise exacerbating
inundation, storm surge,
erosion and other coastal
hazards
Section 4: Projected Trends and Impacts of Climate Change
Source: UNEP 2006, p185
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Reduced freshwater
resources
Invasion by non-native
species
Effects on food and income
security
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“Carbon Crossroads”
Source: Cambridge
University 2013, p 14
Section 4: Projected Trends and Impacts of Climate
Change
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Global Warming by 2100 and Beyond: A Function of Cumulative CO2 Emissions
Section 4: Projected Trends and Impacts of Climate
Change
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Limiting climate
change will require
substantial and sustained reductions of greenhouse
gas emissions.
Source: IPCC 2013, p26
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Sources of Scientific DataSection 5
Module 1: Introduction to Climate Change Science
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The Intergovernmental Panel on Climate Change (IPCC)
Leading body for the assessment of climate change
Established in 1988 by UNEP and WMO
Assesses relevant scientific, technical
and socio-economic information
Does not conduct any research itself
Thousands of scientists from all
over the world contribute to its work
Section 5: Sources of Scientific Data
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Important Reports Published by the IPCC
Assessm
en
t R
epo
rts • First
assessment report (FAR)
• Second assessment report (SAR)
• Third assessment report (TAR)
• Fourth assessment report (AR4)
• Fifth assessment report (AR5)
Specia
l R
epo
rts o
n: • Renewable
energy sources
• Extreme events and disasters
• Emission scenarios
• Aviation
• Carbon capture and storage
Me
tho
do
log
y R
ep
ort
s • Guidance for national greenhouse gas inventories
• Guidance for assessing impacts of climate change
• Land use, land-use change and forestry
Technic
al P
ape
rs • Climate change and water
• Implications of proposed CO2
emissions limitations
• Technologies, policies and measures for mitigating climate change
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Section 5: Sources of Scientific Data
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World Meteorological Organization (WMO) – Global Climate Programmes
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Section 5: Sources of Scientific Data
World Climate Programme (WCP)
World Climate Research Programme
Global Climate Observing System
World Climate Services Programme
Programme of Research on Climate Change
Vulnerability, Impacts and Adaptation
Atmospheric Research and Environment Programme
(AREP)
Global Framework for Climate Services (GFCS)
Advisory Body: Commission for Climatology (CCI)
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In Focus: Global Framework for Climate Services (GFCS)
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URL: http://www.gfcs-climate.org/content/about-gfcs
Section 5: Sources of Scientific Data
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WMO Global Atmosphere Watch: Measurement Stations Worldwide
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Section 5: Sources of Scientific Data
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WMO Regional Climate Centers and Outlook Forums
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Section 5: Sources of Scientific Data
WMO Regional
Climate Centres
(RCCs)
WMO Regional
Climate Outlook
Forums (RCOFs)
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National Climate Data
National
Meteorological and
Hydrological Services
(NMHS)
Collect and manage
national climate data
to help with
forecasting and
predictions
Norfolk Island Meterological Office,
Source: Australian Government: Bureau of
Meteorology
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Section 5: Sources of Scientific Data
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Annex Additional Resources
Module 1: Introduction to Climate Change Science
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Module Summary
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Additional Resources
Weather and climate are the results of complex interactions
between anthropogenic and natural factors.
Evidence of global climate change include higher average
temperatures, changes in precipitation, ocean warming, ocean
acidification, sea level rise, decreasing sea ice, and changes in
physical and biological systems.
Observed climate change can be linked with the increase of
greenhouse gase concentrations in the atmosphere since the
industrial revolution.
Global surface temperature change for the end of the 21st century
is likely to reach 4°C if no drastic mitigation actions are taken.
Various sources of climate data exist that can support planning for
climate change.
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Useful Links
IPCC WebsiteWMO Climate
Pages
Global Framework For Climate
Services (GFCs)
World Climate Programme (WCP)
World Bank Climate Change
Knowledge Portal
NASA Global Climate Change
ESA Climate Change Initiative
NCAR Community Data Portal
Max Planck: The Atmosphere in the
Earth System
The Guardian Climate Change
Pages
The National Geographic -
Global WarmingUN CC:Learn
Additional Resources
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Recommended Readings
Cambridge University (2013). Climate Change: Action, Trends and
Implications for Business
IPCC (2013). Climate Change 2013, The Physcial Science Basis -
Summary for Policymakers
UNEP (2009). Climate Change Science Compendium
UNEP (2009). Climate in Peril, A Popular Guide to the Latest IPCC
Reports
WMO (2013). The Global Climate 2001–2010, A Decade of Climate
Extremes
Additional Resources
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Main References
IPCC (2007). Climate Change 2007 - Synthesis Report
IPCC (2013). Climate Change 2013, The Physcial Science Basis -
Summary for Policymakers
UNEP (2009). Climate in Peril, A Popular Guide to the Latest IPCC
Reports
UNEP (2012). The Emissions Gap Report 2012
WMO (2012): Greenhouse Gas Bulletin
WMO (2009). A History of Climate Activities
WMO Website: Climate
Additional Resources
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