Climate change

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Climate Change – does it really exist? Pavel Alekseychik Khanty-Mansijsk, April 2014 Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

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Transcript of Climate change

Page 1: Climate change

Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

Climate Change – does it really exist?

Pavel AlekseychikKhanty-Mansijsk, April 2014

Page 2: Climate change

Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

Brief CV

• Started at the Russian State Hydrometeorological University (RSHU) at St.Petersburg at 2006

• Continued at the University of Helsinki at 2009, obtained Bachelor’s and Master’s degree there

• Currently at the end of the 3rd year as a PhD student at the group of micrometeorology

• Main interests: biogeochemical cycles in the northern ecosystems, climate-ecosystem interactions, micrometeorology, technology and warfare of the Middle Ages

Page 3: Climate change

Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

“Climate – the history of weather on the timescale of 50 year or longer”

Page 4: Climate change

Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

1. Climate IS changing.

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

Judging by the cave art of Sahara, that place used to beone huge thriving oasis full of life

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

Look at some Dutch Renaissance paintings, 16th – 17th centuries weren’t too warm.

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

You can find a trend in any measurements, like temperature here.So is this showing the changing climate?

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

Periodic climate changes may be found to have affected our civilization

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

Looking at a longer period (Vostok ice core), we still see variation, with a higher amplitude and period

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

Ocean water level is of importance for coastal areas. Not so much for Siberia…

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

The ice ages cause the variation in sea level of more than 100m

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

2. The scale of change

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

It makes a lot of sence to record some quantities for a Long time. You just might see a trend.

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

Add more measurements, and you will see more trends.

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

Derive at what happened to those variables a long time ago,and you will have a better perspective.

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

3. Driving forces behind the climate change

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

Carbon cycle is probably THE main cycle on

earth.

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

A “dead-end” of the carbon cycle: C accumulationIn the form of natural gas/oil/coal

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

Unstable peatland carbon pools

Siikaneva peatland, Finland

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

Unstable peatland carbon pools

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

Some microbes living in peat exhale CH4; industry also does thatCH4 produces a much stronger heating effect than CO2.

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

Methane emissions from natural ecosystems are Strongly controlled by temperature, but what has caused this rise in

the last 300 years?

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

Tectonic activity - a rare, but crucial force[Siberian trapps, thought to have triggered the Permian climate

change and extinction event]

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

Tectonic activity - a sporadic, but crucial force

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

Milankovitch cycles: Earth orbital changes are correlated with its climate

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

4. The climate is constantly adjusted by the greenhouse effect

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

Greenhouse effect

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

IPCC assessment

of effectson climate

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

IPCC: real people

Timo VesalaSigrid DengelMartin HeimannJouni RäisänenVeli-Matti Kerminen…

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

5. But it’s not just about carbon cycle… - feedbacks!

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

BVOC emissions by the forest- biological volatile organic compounds

BVOC

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

BVOC seen as “blue haze”

BVOC

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

Feedback loop:rising CO2 leads to lower temperature??

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

ALBEDO effect:snow masking

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

Interhemispheric CO2 differenceversus anthropogenic emissions

Anthropogenic Emissions of CO2

CO2 (Northern)-CO2 (Southern)

Ref.: Prof. Martin Heimann

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk

5. Synthesis: use all the known relations to predict the future climate

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Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk