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The influence of change at high altitude and high latitude

Raino Heino Finnish Meteorological Institute

CONTENTS

- Background and sources

- Climate changes (past and future) - …. and their impacts - ……. at high latitudes/ altitudes - Concluding remarks WG1 WG2 WG3 References

Intergovernmental Panel on (IPCC) 2007 >3000 p

Impacts of Europe’s changing climate (EEA) Arctic Climate Impact Assessment (ACIA)

etc… EEA ACIA 2009 several 2004 ~2013 WMO - CCl (Commission for Climatology) -IPY (International Polar Year) 2010 - 2012 - CliC (Climate and Crysphere) Springer, 500p

- BALTEX Assessment of Climate Change etc… The Intergovernmental Panel on Climate Change (IPCC) IPCC ja Nobel (2007) was established by WMO and UNEP in 1988 to assess scientific, technical and socio-economic information relevant for the understanding of climate change, its impacts and options for adaptation and mitigation. Main activities and products -> http://www.ipcc.ch IPCC Working Groups /4 major assessment reports -WG I …scientific aspects of climate change - WG II …impacts of climate change… - WG III …mitigating of climate change…

… policymakers need an objective source of information about the causes WHY IPCC ? of climate change, its potential environmental and socio-economic consequences and the adaptation and mitigation options to respond to it.

Rio 1992 Kyoto 1997 Bali 2007 UNFCCC -> Copenhagen 2009

IPCC 1990 IPCC 1996 IPCC 2007 ..…IPCC 2050 Past climate: data sources? Global Tempereture Changes ……in different time-scales…….. Baseline networks of instrumental meteorological data

www.wmo.int -> GCOS Arctic climate information (ACIA)

www.knmi.nl/samenw/eca Spitsbergen Norway Stykkisholmur Iceland Tasillaq Greenland

1800- 1960- 1920-

NORDIC ANNUAL MEAN TEMPERATURES

Stockholm Helsinki

1750- 1840- Arctic vs Global annual temperature anomalies (°C)

Note different scales

IPCC 2007 Warming in the Arctic is >>double that for the globe from 19th to 21st century and from late 1960s to present.

Warmth 1925 to 1950 in Arctic was not as widespread as recent global warmth. BACC: The Baltic area has become warmer… Duration of the ice cover • spring, growing season and summer start earlier in some Finnish lakes • autumn, frost season and winter start later 220 3 Oul uj ärvi 200 2 Annual mean temperature 1 180

0 Kallavesi 160 -1 140 -2 Temperature anomaly ( C) anomaly Temperature -31870 1900 1930 1960 1990 Näsijärvi Duration of ice cover (days) 120

100 North Year Filter South Year Filter 1834 1854 1874 1894 1914 1934 1954 1974 1994

High years Frost Hot precipitation 70 70 days ? days

60 60

50 - 50 +

10 20 30 40 10 20 30 40

Annual trends (days/year) Linear trend in the DJF ECA dataset 1951-2000 number of events above 90th percentile during the period 1958–2000. (BALTEX Assessment of Climate Change….BACC) Interannual variability in water inflow is considerable, but no statistically significant trend is found in the annual time series for the period 1921-2005.

Change -> 2071-2100

1961-90 Large Flood Events 1985-2007

http://www.dartmouth.edu/~floods/Archives

2008 (BALTEX Assessment of Climate Change….BACC)

UNTIL NOW No long-term trends in storminess? However, it is possible to attribute parts - No change in heat of the observed regional changes to content and salinity changes in the large-scale circulation!

- Accelerated rise of the

- Less ice…

Observed Projected IPCC: Past and future? Projections of future temperature changes

Projected warming in 21st century expected to be ”Green” world - greatest over land and at most high northern latitudes Medium - and least over the Southern Ocean and parts of the North Atlantic Ocean ”BaU” Projections of future precipitation changes

Winter Summer

-> Increases very likely in high latitudes -> Decreases likely in most subtropical land regions Implications (… of climate changes) -> IPCC WG2

Arctic ice and snow ..as well as permafrost ..and vegetation zones Ice cover of the Arctic Sea …is disappearing?

??

Thickness2007 2005 Satellite measurements 1966 –July 2008 Snow ?

EU-INTAS project (SCCONE) Snow cover changes over Northern Eurasia

Linear trend coefficients in the time series of mean snow depths for the permanent snow-cover period 1936-2000 IPCC: Glaciers and frozen ground ?

Increased glacier retreat Area of seasonally frozen since the early 1990s ground has decreased… Biological The is ”greening” influences

Flying now in 2100 into climate Climate threat Pine (from satellites) change to coral reefs

Dry Köppen climatic zones Steppe Spruce based on present (1961-90) Desert temperature and precipitation Mild winters* Dry summers Wet all seasons

Birch Cold winters* Dry summers Wet all seasons Polar climates Tundra Ice cap Temp. & Prec. -> 2100

1990s 2050s

2020s 2080s Rising sea levels… 60 cm

IPCC 2007

20 cm Concluding remarks Climate change will not be gradual, but…

Complicated sea currents

Greenland melting

If the Golf stream would not exist! - 5-10 degrC

> 2 km

what about +5 ?

Arctic Climate Impact Assessment (ACIA, 2004) BALTEX Assessment of Climate Change -> BACC (2007)

The overall format is similar to the IPCC - author groups for the individual chapters - overall policymakers-summary - review process.

Springer, 500p

-> http://www.acia.uaf.edu -> http://www.baltex-research.eu ARCTIC:

Present and future temperature (Attribution….)

Natural + anhtropogenic causes

NAO etc?

Natural causes