espere ACCENT online magazine
Printer friendly version of this page
Home    ACCENT Educ.    Science    Encyclopaedia    es    ru    fr    de    it    cn   
Climate Change classes 1
UQ 3 May 07 Cars and ozone
UQ 2 Mar 07 Urban air
Climate change 2007 IPCC special
UQ 1 Nov Dec 06 Particles in air
Special: Oct. 2006 Communication
Nr 10 Sept. 2006 Africa's emissions
Nr 9 July 06 Air traffic
Special: June 06 Climate summit
Nr 8 April 2006 Ozone & N2 cycle
Nr 7 March 2006 Climate modeling
R: Global climate estimation
C: How climate models work
C: Simple models
A: Activities
L: Links
I: Information for teachers
Nr 6 Feb. 2006 acid rain
Nr 5 Jan. 2006 oceanic sulfur
Special: Nov 05 Ozzy Ozone
Nr 4 Oct. 2005 light/satellites
Special: Sept 05 Cyclones
Nr 3 Sept. 2005 methane/energy
Special: July 05 Greenhouse Earth
Nr 2 June 2005 forest/aerosols
No 1 May 2005 vegetation/CO2
     

Download: Word     PDF

research

Climate scenarios for the 21rst century

 How do we know about the future climate?

The Intergovernmental Panel on Climate Change IPCC is a board of climate scientists, politicians and representatives of the economy. Every 5-6 years hundreds of authors from nearly all countries round the world agree on a report, which is organised by about 15 leading authors based on numerous key publications on processes contributing to our climate system and on model results. Such IPCC reports were published in 1990, 1995 and 2001.

 

sea ice simulation

1. Melting of sea ice in the Arctic as simulated in Hamburg: It is expected that the sea ice in summer (light blue) will disappear completely (scenario A1B on the right) or nearly completely (scnario B1 in the middle) compared to current conditions (on the left). MPI Met

For the next report of the IPCC (expected for 2007) several teams of climate modellers have been asked to calculate three "scenarios" for the future climate according to their best knowledge and using the available calculation capacities on super-computers for Earth system modelling. These computers are the largest in the world. One of the teams asked works in the Max Planck Institute for Meteorology in Hamburg, a partner in ACCENT. The results of their calculation will be compared with others. A summarising overview of all results will be shown in the IPCC report. But we can already have a look now at the estimations derived from the climate model in Hamburg. Please note, however, it is only one of 15 teams sending an estimation to the IPCC.
 

 Estimations for the future

Global warming will continue, but not in all regions of the world to the same extent. The landmasses will warm up faster than the oceans. The most notable warming is expected for the northern latitudes and the Arctic regions. Already now we can observe that the Arctic ice, which melts in summer, is not formed anymore in the same volume in winter. By the end of the century the whole Arctic ocean could be ice-free in summer.

2. on the right: Increase of the average temperature on the world for the timespan 2071 - 2100 compared to 1961 - 1990. © MPI Met

 

global temperature increase

Please click the image for a larger version! (90 K)

The intensity of winter storms increases in Central Europe but decreases in the Mediterranean region.

Owing to the warmer air, weather extremes will become more likely. Warm air can hold more water vapour. Therefore, precipitation will increase on average, but not homogeneously spread over the Earth. In humid climate zones like the tropics and mid- and northern latitudes it tends to increase, while the arid zones in the subtropics are becoming drier.
 

extreme precipitation

3. Extreme precipitation: Percent change of extreme precipitation for the period 2071 - 2100 compared to 1961 - 1990. Scenario A1B
Please click the image for a larger version. (20 K)

extreme drought

4. Extreme drought: Percent change of maximum drought periods for the time 2071 - 2100 compared to 1961 - 1990. Scenario A1B. Please click the image for a larger version. (20 K) MPI Met
 

precipitation change

This means the contrast between dry and wet climate zones becomes more pronounced. More severe droughts are expected for the Mediterranean region, South Africa and Australia. In the humid region the risk of heavy rain and floods increases. Winter snowfall decreases by 80-90% in most European countries by the end of the century (30-40% in the Alps and the Norwegian mountains). The length of dry spells increases world-wide.

5. on the left: Changes in precipitation for the period 2071 - 2100 compared to 1961 - 1990 for the months January and July.
Please click the image for a larger version. (115 K) MPI Met
 

sea level change

6. Expected change of the sea level in meters for 2100 compared to the year 2000. Please note that the sea level change is not homogeneous over the whole planet.
Please click the image for a larger version. (80 K) MPI Met
 

The ocean level may rise by 20-30 cm due to the thermal expansion. The melting of Greenland ice will be responsible for another 15 cm while heavier snowfall in Antarctica could lead to a reduction by 5 cm. The melting process in the Arctic causes a strong flux of freshwater into the salty Northern Atlantic ocean. This causes changes in the ocean circulation which is driven by differences in temperature and saltiness. The North Atlantic current could slow down and promote a cooler climate in Europe, which is however outweighed by the general warming trend.

 

Greenhouse warming has been masked in some way by air pollution which has prevented sunlight from reaching the Earth's surface. If strong measures are taken for the improvement of air quality world-wide this could lead to a rapid warming of almost 1C in ten years.

Table 1: The model runs are based on the following carbon dioxide (CO2) and sulphur dioxide (SO2) emissions:
CO2 SO2 table

Nowadays climate models also include sulphur emissions, which make a major contribution to air pollution, aerosol formation and backscattering of sunlight. This masks the global warming.

The predicted further warming until 2100 will be in the range of 2.5 - 4C on average.

 

 Scenarios

The result of the model depends on the scenario the calculations are based on. The IPCC developed different scenario families for the future, which have been the basis for this calculation. They are called A1, A2 and B1 and they depend on different assumptions for the demographic, social, economic and technological development of our world.

 

temperature trend

8. Trend in the temperature relative to a zero-line for the average temperature 1961 - 1990. The deviation in the temperature development for the different scenarios is relatively small. The reason is that in scenarios of better technological improvement the cooling effect of air pollution is removed earlier and outweighs slightly the advantage of lower CO2 emissions.
Please click the graph for a larger version. MPI Met

The family A2 describes a heterogeneous development. Population and economic growth vary strongly in different regions in the world. Therefore the population continues to rise and the development in income per capita and technological change differ a lot and develop slowly. This scenario promotes climate change more strongly than the others.

The family A1 describes a world with strong economic growth and a population reaching its maximum around 2050. The introduction of new technologies is quick and efficient. But the growth can be based on different resources: intensive use of fossil fuels (A1F), of non-fossil energy resources (A1T) or on mixture of both (A1B). Since the present trends go into the direction of an A1B scenario it is popular as an example. But certainly there is no guarantee how the world will develop in the coming decades.

The family B1 assumes a population development like in A1 but the society will be very soon based on information technologies and services. The intensity of material and energy usage is reduced based on intelligent systems and sustainable policy and economy. Social balance and global justice increases but the scenario does not include specific climate protection programs.

 

CO2 trend

 

 

The scenario B1 is the best for our climate but even in this case the CO2 level will reach about 550 ppm at the end of the century, which is a doubling compared to the pre-industrial value of 280 ppm.

9. on the left: CO2 mixing ratios - observed from 1850 - 2000 and estimated for different IPCC scenarios until 2100.
Please click the graph for a larger version. MPI Met

 

 

Author: Elmar Uherek - Max Planck Institute for Chemistry, Mainz
English check: Mark Jacob, TU Freiberg

The background information for this text and all illustrations were taken from a brochure published in German by the Max Planck Institute for Meteorology in Hamburg.

Texts: Erich Roeckner, Guy P. Brasseur, Marco Giorgetta, Daniela Jacob, Johann Jungclaus, Christian Reick, Jana Sillmann
Graphics: Norbert P. Noreiks

 top

ACCENT / ESPERE

last updated 17.04.2008 | © ACCENT - Atmospheric Composition Change 2013