Climate change
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Transcript of Climate change
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
Climate Change – does it really exist?
Pavel AlekseychikKhanty-Mansijsk, April 2014
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
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
“Climate – the history of weather on the timescale of 50 year or longer”
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
1. Climate IS changing.
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
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
Look at some Dutch Renaissance paintings, 16th – 17th centuries weren’t too warm.
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?
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
Periodic climate changes may be found to have affected our civilization
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
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
Ocean water level is of importance for coastal areas. Not so much for Siberia…
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
The ice ages cause the variation in sea level of more than 100m
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
2. The scale of change
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.
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
Add more measurements, and you will see more trends.
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.
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
3. Driving forces behind the climate change
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
Carbon cycle is probably THE main cycle on
earth.
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
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
Unstable peatland carbon pools
Siikaneva peatland, Finland
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
Unstable peatland carbon pools
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.
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?
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]
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
Tectonic activity - a sporadic, but crucial force
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
Milankovitch cycles: Earth orbital changes are correlated with its climate
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
4. The climate is constantly adjusted by the greenhouse effect
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
Greenhouse effect
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
IPCC assessment
of effectson climate
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
IPCC: real people
Timo VesalaSigrid DengelMartin HeimannJouni RäisänenVeli-Matti Kerminen…
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
5. But it’s not just about carbon cycle… - feedbacks!
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
BVOC emissions by the forest- biological volatile organic compounds
BVOC
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
BVOC seen as “blue haze”
BVOC
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
Feedback loop:rising CO2 leads to lower temperature??
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
ALBEDO effect:snow masking
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
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk
5. Synthesis: use all the known relations to predict the future climate
Pavel Alekseychik, University of Helsinki 2 April 2014, Khanty-Mansijsk