ian james diocese of oxford e-mail. environment advisor [email protected] climate change...

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Ian James Diocese of Oxford E-mail . Environment Advisor [email protected] Climate change Climate change Revd Professor Ian James Head of School of Mathematics, Meteorology & Physics, University of Reading Oxford Diocesan environment advisor [email protected] om

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Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

Climate changeClimate change

Revd Professor Ian JamesHead of School of Mathematics, Meteorology &

Physics, University of Reading

Oxford Diocesan environment advisor

[email protected]

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

Plan of talkPlan of talk

• The problem

• Is climate change real?

• Some complications

• The future

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

The problemThe problem

- why climate change is a concern

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

Atmospheric carbon dioxideAtmospheric carbon dioxide

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

A little goes a long way!A little goes a long way!

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

Two views of EarthTwo views of Earth

Visible light Infra-red view

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

The “greenhouse” effectThe “greenhouse” effect

• Carbon dioxide blankets Earth’s surface.

• Sunlight gets in.

• Infra-red absorbed and re-emitted.

• Other greenhouse agents – water vapour, clouds.

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

Carbon dioxide & ice agesCarbon dioxide & ice ages

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

The carbon cycleThe carbon cycle

• Fossil fuels (coal, oil, natural gas) are made of carbon and hydrogen.

• When burnt, they produce energy, water and carbon dioxide.

Human Natural

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

What activities generate What activities generate carbon dioxide?carbon dioxide?

• All sources are comparable

• No easy target!• Reduction across

the board

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

Is climate change happening?Is climate change happening?

Some examples

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

Variations of the Earth’s surface temperature for the past 1,000 years

SPM 1b

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

Summer 2003Summer 2003

Deviation from 1961-1990 mean

Based on ECMWFand ERA-40

Color: temperature anomaly

Contours: normalized by standard deviation

(Schär et al. 2004, Nature, 427, 332-336)

ºC

Temperature Anomaly June-August 2003

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

HurricanesHurricanes

•More intense

•More extremes

•Form over hottest sea

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

Arctic sea iceArctic sea ice

September 1979 September 2005

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

Glaciers in retreatGlaciers in retreat

Pasterze glacier, Austria, 1875 Same view, 2004

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

Sea-level transgression scenarios for BangladeshSea-level transgression scenarios for Bangladesh

Adapted from Milliman et al. (1989).

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

Some complications….Some complications….

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

Feedbacks……Feedbacks……

A positive feedback loop…

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

Examples of climate feedbacksExamples of climate feedbacks

• Warm atmosphere becomes moister

• Melting ice & snow makes surface darker

• Melting tundra releases methane

• Moist atmosphere becomes cloudier

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

Melting permafrostMelting permafrost

• Vast areas of the high northern latitudes have permanently frozen soils – “tundra”.

• These are thawing out as warming accelerates

• Thawing releases methane• Methane is an even more

potent greenhouse gas than carbon dioxide

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

The “tipping point”The “tipping point”

• The point at which carbon dioxide levels are so high enough that feedbacks take over, and changes become irreversible.

• Are we approaching a “tipping point”?

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

The future?The future?

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

Global carbon emissions from fossil fuelsGlobal carbon emissions from fossil fuels

Ian James Diocese of Oxford E-mail . Environment Advisor [email protected]

Only connect!Only connect!

• Interdependence of natural world

• We are part of natural world!

• Need to live sustainably within the entire world community