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Table 3 Major Impacts of Climate Change on the Earth System
| Temp- | [CO2] | Year in Impacts to the earth system | Region | Source | |
| erature | ppm | which | affected | ||
| rise | impact | ||||
| above | occurs | ||||
| prein- | |||||
| dustrial | |||||
| OBSERVED CHANGE | |||||
| 0.6 | 378 | 2004 | Annual average temperature | Globe | IPCC TAR |
| has risen by 0.6C | |||||
| 0.6 | 2004 | Temperature has risen by | Arctic | ACIA 2004 | |
| 1.8C; could rise by 10C by | |||||
| 2100 | |||||
| 0.6 | 2004 | Sea surface temperature | Globe e.g. N | IPCC 2001; | |
| increased by 0.6C +/-0.1C | Sea where | EEA 2004 | |||
| 0.5C rise in | |||||
| 15 years | |||||
| 0.6 | 2004 | 90% globe’s glaciers | Globe e.g. | EEA 2004, | |
| retreating since 1850 (not | Alps where | Street & | |||
| attributed) | 70-90% mass | Melnikov | |||
| loss (30-40% | 1990 | ||||
| since 1980) | |||||
| 0.6 | 2004 | Increased freshwater flux | Northern and | ECF 2004 | |
| from Arctic rivers appears to | Western | ||||
| be already 20% of what | Europe | ||||
| would cause shutdown of | |||||
| THC | |||||
| 0.6 | 2004 | Arctic sea ice extent | Arctic | Cavalieri et | |
| decreased by 0.30 +/- 0.03 x | al 2003 | ||||
| 10 6 km(2)/10 yr from 1972 | |||||
| through 2002, but by 0.36 +/- | |||||
| 0.05 x 10(6) km(2)/10yr from | |||||
| 1979 through 2002, indicating | |||||
| an acceleration of 20% in the | |||||
| rate of decrease. | |||||
| 0.6 | 2004 | 3.7+/- 1.6C warming/century | Antarctic | Vaughan et | |
| observed | Peninsula | al 2003 | |||
| 0.6 | 2004 | N hemisphere snow cover | N | EEA 2004 | |
| decreased by 10% since 1966 | hemisphere | ||||
| 0.6 | 2004 | Measured spring snowpack | Switzerland | Scherer et al | |
| decreased in Alps | 2004 | ||||
| 0.6 | 2004 | Measured spring snowpack | Cascades & | Mote 2005 | |
| declined, (not attributed) | N California, | ||||
| correlated with rising | USA | ||||
| temperature/declined | |||||
| precipitation | |||||
| 0.6 | 2004 | Arctic sea ice reduced by 15 - | Arctic | ACIA 2004 | |
| 20% | |||||
| 0.6 | 2004 | Bottom melt rates of | Antarctic | Rignot & |
| Antarctic glaciers increase by | Jacobs 2002 | |||
| 1m/year for each 0.1C rise in | ||||
| ocean temperature | ||||
| 0.6 | 2004 | Some evidence that | Amazon | ECF 2004 |
| savannaisation of parts of | ||||
| Amazon triggered by land use | ||||
| change interacting with | ||||
| warming | ||||
| 0.6 | 2004 | Greenland ice sheet losing | Greenland | Rignot & |
| mass (not attributed) | Jacobs 2002 | |||
| 0.6 | 2004 | West Antarctic Ice Sheet | Antarctic | Rignot & |
| losing mass overall; | Jacobs 2002 | |||
| 0.6 | 2004 | Larsen B ice shelf collapse; | Antarctic | Rignot et al |
| subsequent ice discharge from | 2004 | |||
| land (not attributed) | ||||
| 0.6 | 2004 | Increase in global sea level | Globe | Thomas et al |
| of 1.8 mm/year : about 50% | 2004 | |||
| of this caused by melting of | ||||
| terrestrial ice (remainder | ||||
| from thermal expansion of | ||||
| water), of which 0.4 mm/yr | ||||
| from non-polar glaciers, 0.4 | ||||
| mm/yr from Greenland, | ||||
| estimated 0.2 mm/yr from | ||||
| West Antarctic Ice Sheet | ||||
| 0.6 | 2004 | Green biomass increased by | Europe | EEA 2004 |
| 12% (not attributed) | ||||
| PREDICTED CHANGE | ||||
| 1.5 | 7m sea | Onset of complete melting of | All coastal | Gregory |
| level | Greenland ice: when | regions; | 2004 | |
| rise | complete 7 m of additional | many world | ||
| over | sea level rise | cities | ||
| betwee | inundated | |||
| n x and | ||||
| y years | ||||
| 2 – 3?? | CO | Collapse of Amazon | S America, | Cox et al |
| 2doubli | rainforest replacing forest by | also globe | 2004, Betts | |
| ng +/- | savannah: enormous | 2005 | ||
| ?q | consequences for biodiversity | |||
| and human livelihoods | ||||
| 2 to 3? | 550 +/- | Conversion of terrestrial | Global | Cox et al |
| ?? but | carbon sink to carbon source, | 2000, Cox | ||
| inevita | due to temperature-enhanced | 2005, ECF | ||
| ble at | soil and plant respiration | 2004 | ||
| some | overcoming CO2-enhanced | |||
| point | photosynthesis. Resulting in | |||
| desertification of many world |
Regions as there is widespread loss of forests and grasslands, and accelerating warming through a feedback effect
| Any | Release of C to atmosphere | Global | Neilsen 1993 | ||
| due to deterioration of | |||||
| ecosystems at rapid rates of | |||||
| temperature change | |||||
| Double | Net primary production | Globe | Betts 2005 | ||
| increases by 10% | |||||
| Double | Runoff increases by 12% | Globe | Betts 2005 | ||
| 2.3 | 2100 | Collapse of thermohaline | Globe; | Schlesinger | |
| circulation: Maximum | cooling NW | 2005 | |||
| likelihood of shutdown of 4 in | Europe, | ||||
| 10 for climate sensitivity of | warming | ||||
| 3C (and climate sensitivity | Alaska and | ||||
| could lie between 1.5 and | Antarctic, | ||||
| 11C) | decreasing | ||||
| rainfall in S | |||||
| America | |||||
| 1.5 | Probability of collapse | Yohe, | |||
| exceeds 50% | Schlesinger | ||||
| and | |||||
| Andronova | |||||
| in press. | |||||
| 1 – 3 | Collapse of thermohaline | Northern and | Rahmsdorf | ||
| circulation affecting fisheries, | Western | in ECF 2004 | |||
| ecosystems, agriculture: | Europe | ||||
| expert opinion probabililty “a | |||||
| few percent” | |||||
| 3 | 2100 | 700 | THC collapse | O’Neill & | |
| Oppenheime | |||||
| r 2002; | |||||
| Keller et al | |||||
| 2004 | |||||
| 2 – 4.5 | Potential to trigger melting of | Globe | ECF 2004 | ||
| the West Antarctic Ice Sheet | |||||
| raising sea levels by a further | |||||
| 5 to 6 m ie 60 to 120 | |||||
| cm/century | |||||
| 4 – 5 | Expert opinion: probability of | Northern and | Rahmsdorf | ||
| thermohaline shutdown up to | Western | in ECF 2004 | |||
| or above 50% | Europe | ||||
| Comme | THC collapse, Greenland Ice | Discussed at | |||
| nt: | Sheet melt and West | conference | |||
| Antarctic Ice Sheets may | |||||
| interact in ways that we have | |||||
| not begun to understand | |||||
| Potential release of methane | Globe: | IPCC 2001 |
| from melting tundra and | feedback | ||
| clathrates from shallow seas; | accelerating | ||
| add recent publication | warming | ||
| mentioned at conference that | |||
| we may be nearing this point | |||
| 2100 | Acidification of the oceans | World | IPCC 2001; |
| falls by 0.4: may disrupt | oceans | Blackford | |
| marine ecosystem | 2005; Archer | ||
| functioning, in turn reducing | 1995 | ||
| buffering capacity of oceans | |||
| (positive feedback) | |||
| 2250 | Acidification falls by 0.77 | World | IPCC 2001; |
| oceans | Blackford | ||
| 2005 | |||
| Increased variability in | Asia, | IPCC 2001, | |
| summer monsoons | Australia | Steffen 2005, | |
| exacerbating flood/drought | Lal 2003 | ||
| damage | |||
| 16 | Permanent El Nino | Globe | Navarra |
| xCO2 | 2005 |
*Note: at 0.6C some observed changes are marked as “not attributed”. In these cases calculations of the cause of these changes has not yet been made. They are listed because they are changes which are consistent with the patterns of change predicted to result from anthropogenic climate change.