24 April 2014 The Great Channel 4 Swindle Robin Hogan Thanks to: Jonathan Gregory, Giles Harrison and Peter Stott Return.

Slides:



Advertisements
Similar presentations
Volcanoes Large volcanic eruptions with high SO2 content can release SO2 into the stratosphere. This SO2 eventually combined with water vapor to make.
Advertisements

Earths Climate System Dr. R. M. MacKay. Natural and Anthropogenic Climate Forcing.
The solar spectrum compared to a black body. Sun ~6000K Sun radiates a lot more energy that the Earth! Earth ~290K Blackbody radiation curves typical.
Climate Change & Global Warming: State of the Science overview December 2009 Nathan Magee.
Pacific Northwest Weather and Climate, Past, Present and Future George H. Taylor October, 2007.
 Extends from the Earth’s surface to outer space.  About 900 km (560 miles)  Mixture of gases, solids, and liquids.
CALEB BRITISH ACADEMY LAGOS NIGERIA. Earth’s temperature depends on the balance between energy entering and leaving the planet’s system.energy entering.
Climate Change. Climate change: Changes in many climatic factors. Global warming: The rise in global temperatures.
Global Greenhouse Effect (steady-state) vs. Global Warming (disturbed steady-state)
9 November 2002The North Texas SkepticsJohn Blanton, Curtis Severns Global Warming Science Solar Radiation Ozone and Oxygen absorb nm. Water.
SC.912.E.7.7 Identify, analyze, and relate the internal (Earth system) and external (astronomical) conditions that contribute to global climate change.
Solar Radiation: The driving factor Radiation (energy transmitted as waves, rays and particles) released, absorbed & reflected by all things travels as.
What do Greenhouse Gases Do? Kevin Czajkowski University of Toledo
The Atmosphere “Vapor Globe/Ball”. Composition  78% Nitrogen  21% Oxygen  1% Other (Argon, Carbon Dioxide, Water Vapor, other gases)  78% Nitrogen.
Composition  Nitrogen (N 2 ): 78%  Oxygen (O 2 ): 21%  Other Gases: 1% Argon (Ar): 0.934% Carbon Dioxide (CO 2 ): 0.037% Water Vapor (H 2 O): 0.01.
Chapter 11 Heating the Atmosphere. Weather and Climate  Weather  Weather is over a short period of time  Constantly changing  Climate  Climate is.
Weather Condition of the atmosphere at any particular time and place Air temperature, air pressure, humidity, clouds, precipitation, visibility, wind Climate.
Monday, 8/31/091 ATMO Class #2 Monday, August 31, 2009 Chapter 1 Introduction to the Atmosphere.
temperatures-ice.html 2009/3/26 Pei-Yu Chueh CO 2 vs temperature: ice core correlation & lag Lubos.
Insolation and the Seasons Unit 6. Solar Radiation and Insolation  Sun emits all kinds of E E.  Most of the E E is visible light.  Sun emits all kinds.
Radiation in the Atmosphere. Gases can absorb AND give off radiation. Objects around you look bright on a sunny day. Earth’s atmosphere reflects or absorbs.
Global Warming Cause for Concern. Cause for Concern? What is the effect of increased levels of carbon dioxide in the Earth’s atmosphere? Nobody knows.
Sustainability and Globalization Global Warming. A global issue with regards to sustainability A world-wide warming of the Earth’s lower atmosphere.
Anthropogenic Climate Change. Global Temperature is Increasing.
24 Global Ecology. Global Biogeochemical Cycles Atmospheric CO 2 affects pH of the oceans by diffusing in and forming carbonic acid.
The Atmosphere.
Carbon Dioxide CO 2 RF = 1.66 W/m 2. Methane CH 4 RF = 0.48 W/m 2.
Temperature Anomaly (  C) Annual Solar Radiation (W m -2 )
Physics of Planetary Climate Cors221: Physics in Everyday Life Fall 2010 Module 3 Lecture 8: Climate During This Interglacial.
Human fingerprints on our changing climate Neil Leary Changing Planet Study Group June 28 – July 1, 2011 Cooling the Liberal Arts Curriculum A NASA-GCCE.
Conversations with the Earth Tom Burbine
FGHALL1 Greenhouse Gases Carbon dioxide CO 2 Methane CH 4 Water Vapor H 2 O Nitrous Oxide N 2 O Chloroflorocarbons CFC’s Ozone O 3 Absorbing Aerosols Smoke.
TOPIC III THE GREENHOUSE EFFECT. SOLAR IRRADIANCE SPECTRA 1  m = 1000 nm = m Note: 1 W = 1 J s -1.
Climate Change: Causes and Evidence Part 1.. Climate Change What is the cause? How do we know? What is the Keeling Curve? How much CO 2 is in the atmosphere.
1 Radiative Forcing The balance between incoming solar radiation and heat radiation leaving the atmosphere.
MonthDayLectureActivityChap. Nov.21Ecosystems IIServices56 26Global C cycle56 Dec.3Thinking ecologically I 5Thinking ecologically II Eco. literacy 10Exam.
17.1 Atmosphere Characteristics
AAAHHHHH!!!!. Climate Change Climate Physical properties of the troposphere of an area based on analysis of its weather records over a long period Two.
Greenhouse Gases Current Weather Anthropogenic Influences on Climate Why are Greenhouse Gases Important? Carbon Dioxide, Methane, and Nitrous Oxide Radiative.
Section 1.3 Gases in the atmosphere absorb radiation.
Composition of the Atmosphere 14 Atmosphere Characteristics  Weather is constantly changing, and it refers to the state of the atmosphere at any given.
L’effetto serra e il riscaldamento globale. Structure of the Atmosphere Thermosphere Mesosphere Ozone Maximum Stratosphere Troposphere Temperature.
The Greenhouse Effect on Climate Change.  1. The sun’s rays warm up the land and the water.  2. Infrared rays bounce back to space.  3. Some are trapped.
Section 3.2 The Atmosphere
Aim: How do increased carbon dioxide concentrations on our planet affect life?
To recap Give 2 examples of research methods that show long term historical climate change? How reliable are these? Give 2 ways of measuring medium term.
Solar Radiation: The driving factor Radiative Energy (energy transmitted as waves, rays and particles) released, absorbed & reflected by all things travels.
Solar Radiation: The driving factor
The Greenhouse Effect 8.6 The greenhouse effect is a natural process whereby gases and clouds absorb infrared radiation emitted by Earth’s surface and.
The Sun and the Earth’s Climate
Greenhouse Effect and Global Warming
Chapter 19 Global Change.
History, Structure and Composition of the Atmosphere
Radiation in the Atmosphere
Gases in the Atmosphere absorb Radiation
Global Warming Effects of increase CO2
Earth's atmosphere reflects or absorbs some sunlight but allows most of the visible light pass through to Earth's surface. 4 ways the atmosphere affects.
Human Activities and Climate Change
The Sun and the Earth’s Climate
Radiation in the Atmosphere
Are You Smarter Than a 9th Grader?
Climate, Energy, and Earth
NATURAL CAUSES OF CLIMATE CHANGE
Intro to Climate Change
History, Structure and Composition of the Atmosphere
The Sun and the Earth’s Climate
Wind scale. Wind scale Global warming - increased surface temperature due to natural and man-made causes. But……what’s the problem? Questions: 1)
The Sun and the Earth’s Climate
Characteristics of the Atmosphere
Characteristics of the Atmosphere
Presentation transcript:

24 April 2014 The Great Channel 4 Swindle Robin Hogan Thanks to: Jonathan Gregory, Giles Harrison and Peter Stott Return

24 April 2014 Overview The following claims were made in The Great Global Warming Swindle produced by Martin Durkin: Concentrations of CO 2 are too small to be important CO 2 doesnt match 20th century temperature record It can all be explained by sunspots The troposphere isnt warming Volcanoes emit far more CO 2 than humans

24 April 2014 Concs of CO 2 (~300ppmv) are too small But the per-molecule absorption cross-section of CO 2 is hugely greater than N 2 and O 2 in the infrared Carbon dioxide absorption in the middle of the infrared spectrum …a daft comment anyway: 300 ppmv of HCN is lethal, so why shouldnt 300 ppmv of CO 2 be important?

24 April 2014 CO 2 doesnt match temperature ?

24 April 2014 Whoever said only CO 2 affects climate? Anthropogenic forcings Carbon dioxide and other gases Tropospheric aerosol emissions Land use changes Natural forcings with an established mechanism Stratospheric aerosol (volcanoes) Solar irradiance changes Changes to Earths orbit (Milankovic cycles) (~20 kyr) Solar cycle effect on ozone via UV modulation (11 yr) Possible natural forcings lacking an established mechanism Cosmic ray effects on clouds (11 or 22 yr?) Solar system and galactic spiral arms (~0.5 Gyr) And natural variability!

24 April 2014

Official NASA data have an earlier upturn ? ??

24 April 2014 From The Independent Source of Channel 4 temperature plot 1998 article in Medical Sentinel by known climate sceptics From NASA but Northern hemisphere land (<1/3 of globe) Ended in the early-1980s so underplayed recent warming Martin Durkin admitted that his graphics team changed the scale so that it extended to 2000! Durkin quotes on the matter there was fluff there the original Nasa data was very wiggly-lined and we wanted the simplest line we could find

24 April 2014

Shape of temperature rise can be calculated by considering natural and anthropogenic forcings Post-war economic boom led to aerosol emissions, initially offsetting the CO 2 forcing Pinatubo 1991 El Chichon 1982 Agung 1963

24 April 2014 More recently: IPCC 2007 Solar irradiance + volcanoes Carbon dioxide + aerosols All

24 April 2014 It can all be explained by solar-cycle length

24 April 2014 Friis-Christensen & Lassen (1991) Smoothed solar-cycle length Un-smoothed points (end of time series as of 1991) Corrected by Damon and Laut (2004) When the new data became available: Lassen and Friis-Christensen 2000

24 April 2014 Solar cycle length clearly cannot explain the last 50 years of warming But discredited data still used in C4 programme! Note that we can predict temperature change due to CO 2, but cosmic ray link is currently just a correlation: mechanism is uncertain Damon and Laut (2004) Upturn previously used to explain recent warming now looks like a blip!

24 April 2014 Longer periods… ?Problems with fitting: Maunder minimum filled in with perfectly correlated data Two temperature series were spliced together at 1870, but lowering the second by 0.1 degrees! The result looks less convincing when these effects are corrected

24 April 2014 But lots of temperatures to chose from! Key point: no change in solar activity has been observed that could explain the warming in the last few decades Note that changes to the solar irradiance are important at certain times (e.g. beginning of 20th century), but these are correlated to sunspot number so we must be very careful in attribution of correlations of temperature with solar activity

24 April 2014 Troposphere should warm faster than surface This is consistent with recent analysis of satellite Microwave Sounding Unit (MSU) Christy and Spencer (2003) analysis indicated troposphere warming slower than surface Mears and Wentz corrected for diurnal drift of satellite: there is now consistency with theory

24 April 2014 IPCC verdict IPCC 2007: New analyses of balloon-borne and satellite measurements of lower- and mid-tropospheric temperature show warming rates that are similar to those of the surface temperature record and are consistent within their respective uncertainties, largely reconciling a discrepancy noted in the TAR*. *TAR = Third Assessment Report, IPCC 2001

24 April 2014 Volcanoes emit more CO 2 than humans Steady outgassing: up to 0.2 GtC/yr (Morner and Etiope 2002), but IPCC 2001 has < 0.1 (cf. anthropogenic: 6 GtC/yr) How much is emitted in a volcanic eruption? Pinatubo 1991 El Chichon 1982 Agung 1963 …and Mauna Loa is itself a volcano!

24 April 2014 Return Useful links RealClimate John Houghtons site The Independent Point-by-point rebuttal The graphs from the programme