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Climate science overview

Climate science overview. Andrew Ash . Brisbane, 14 June 2006. Outline. Evidence for climate change Projections for the 21 st century Potential impacts. Outline. Evidence for climate change Projections for the 21 st century Potential impacts.

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Climate science overview

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  1. Climate science overview Andrew Ash Brisbane, 14 June 2006

  2. Outline • Evidence for climate change • Projections for the 21st century • Potential impacts

  3. Outline • Evidence for climate change • Projections for the 21st century • Potential impacts

  4. Climate has always been variable. Ice ages occur every 100,000 years due to wobbles in the Earth’s orbit. Greenhouse gases and ice sheets enhance the orbital effect on temperature by about 50% ? The present CO2 level is unprecedented in at least the past 420,000 years and it is expected to rise to 550-950 ppm by the year 2100 Temperatures may rise by 1.4-5.8oC by 2100

  5. In the past 200 years, concentrations of greenhouse gases have continued to increase, and the Earth has warmed. This is the enhanced greenhouse effect The main greenhouse gases are water vapour, carbon dioxide, methane, nitrous oxide, ozone and CFCs Since 1750, carbon dioxide has risen 35%, methane 151%, nitrous oxide 17%, tropospheric ozone 36% The temperature of the late 20th century is the highest in at least the past 1000 years

  6. In the past 100 years, global average surface temperatures have risen 0.7ºC Difference from 1961-1990 average (oC) 1860 1880 1900 1920 1940 1960 1980 2000 The 12 warmest years on record have occurred since 1990(WMO, 2005)

  7. Over the past 50 years, global average sea-level has risen 9 cm (1.85 mm/year) Source: Church et al (2004)

  8. Other evidence • Warming of the upper 300 m of ocean • Warming in the lowest 8 km of atmosphere • Increase in extremely high temperatures, decrease in extremely low temperatures • More-intense rainfall and cyclones in many places • Oceans are becoming more acidic due to higher CO2 • Snow cover and ice extent have decreased • Shifts in plant and animal locations and behaviour • In Australia • Warming of 0.9oC since 1910, mostly since 1950 • Min temps rising faster than max temps • More heatwaves and fewer frosts • More rain in the north-west, less in south and east since 1950 • Less extreme rainfall in the south and east since 1950

  9. Causes of climate change • Global warming in the early 20th century was mostly due to natural variability, e.g. solar variations and volcanic eruptions • Most of the global warming of the past 50 years is due to human activities that have increased greenhouse gases, aerosols and ozone depletion • In Australia, most of the warming is due to human activities • There is uncertainty about the causes of Australian rainfall trends • Increases in the northwest may be due to natural variability and a shift in weather patterns due to increases in northern hemisphere aerosols • Decreases in the south may be due to natural variability, increases in greenhouse gases and ozone depletion • Decreases in the east are due to an increase in El Niños since 1975, the cause of which is unknown

  10. Most of the observed warming over the last 50 years is attributable to human activities that have increased greenhouse gas concentrations GHGs, aerosols, ozone depletion Solar & volcanic

  11. Outline • Evidence for climate change • Projections for the 21st century • Potential impacts • Action

  12. Climate change projections • Rather than simply extrapolating observed trends, we use computer models of the climate system driven by scenarios of greenhouse gas and aerosol emissions, and ozone depletion • Emission scenarios have various assumptions about demographic, economic and technological change

  13. Climate change projections • Global warming of 0.5-1.2oC by 2030 and 1.2-3.8oC by 2070 • Sea level rise of 3-17 cm by 2030 and 7-50 cm by 2070 • In Australia • Warming of 0.5-2oC by 2030 and 1-6oC by 2070 • Less frost and snow, more heatwaves and fires • Less annual total rainfall over southern and eastern Australia • More frequent and intense droughts • Increases in intensity of rain, floods, tropical cyclones and storm surges

  14. 2030 projections for south-eastern Qld b Results for 2040 (changes for 2030 not available) For risk assessment, it is important to consider extreme scenarios, even though they may have low probability (this is why we have insurance). Note the high global warming including the uncertainty, e.g. annual average rainfall may decline by almost 15% and evaporation may rise by 10%

  15. 2030 projections for north-eastern Qld b % changes are not provided for seasons with very low rainfall C Results for 2050 (changes for 2030 not available) For risk assessment, it is important to consider extreme scenarios, even though they may have low probability (this is why we have insurance). Note the high global warming including the uncertainty, e.g. annual average rainfall may decline by almost 15% and evaporation may rise by 7.5%

  16. Outline • Evidence for climate change • Projections for the 21st century • Potential impacts • Action

  17. Potential impacts without adaptation • Key conclusions for Australia • Most vulnerable ecosystems are wet tropics, Kakadu, alpine areas, coral reefs, freshwater wetlands, and heathlands in south-western Australia • Generally less stream flow in southern and eastern Australia • Crops may benefit from warmer conditions and higher CO2 but this may be offset by reduced rainfall • Greater exposure of infrastructure to extreme weather events and sea-level rise • Greater exposure to heat-related deaths and dengue fever • A few examples follow for Queensland

  18. Water • Water resources are likely to be further stressed due to projected growth in demand and climate-driven changes in supply for irrigation, cities, industry and environmental flows • A decline in annual rainfall with higher evaporative demand would lead to less run-off into rivers, e.g. e.g. -15% to +5% in the Fitzroy River • Droughts are likely to become more frequent and more severe • Fire risk is likely to rise, affecting water yield and quality in fire-affected catchments

  19. Heat • Queensland is likely to become warmer, with more hot days and fewer cold nights • Average number of days above 35ºC • Cairns Townsville Longreach Brisbane Charleville • Now 3 4 115 3 65 • 2030 4-14 5-18 129-163 3-6 76-106 • Increased peak summer energy demand for cooling is likely, with reduced energy demand in winter for heating • Warming and population growth may increase annual heat-related deaths in those aged over 65, e.g. from 134 deaths at present in Brisbane to 165-189 by 2020 and 776-1368 by 2050 • Higher temperatures may also contribute to the spread of vector-borne, water-borne and food-borne diseases, e.g. the mosquito that carries Dengue Fever may reach Rockhampton by 2050

  20. Agriculture • Controlled experiments have shown grain yield increases under elevated atmospheric carbon dioxide concentrations. However, it is not known whether this will translate to field conditions in Australia due to nutrient limitations and elevated temperatures. • Low to moderate warming may also help plant growth especially frost sensitive crops such as wheat, but more hot days and a decline in rainfall or irrigation could reduce yields. Warmer winters can reduce the yield of stone fruits that require winter chilling and grape quality is likely to decline. • Livestock would be adversely affected by greater heat stress. • In forestry, the CO2 benefits may be offset by decreased rainfall, increased bushfires and changes in pests.

  21. Cities • Changes in average climate and sea-level will affect building design, standards and performance, energy and water demand, and coastal planning • Increases in extreme weather events are likely to lead to increased cyclone damage, flash flooding, strains on sewerage and drainage systems, greater insurance losses, possible black-outs, more fires and challenges for emergency services.

  22. Ecosystems • Corals on the Great Barrier Reef would be exposed to annual bleaching by 2030 (high global warming) or by 2050 (medium global warming). Given that the recovery time from a severe bleaching event is at least 10 years (50 years for full recovery), reefs may be dominated by non-coral organisms such as macroalgae by 2050. • Substantial impacts on biodiversity, fishing and tourism are expected. • The distribution of rainforest types in North Queensland Wet Tropics may increase or decrease with warming, depending on the direction of rainfall change

  23. Concluding remarks Climate change is real and underway Most of the warming of the past 50 years is due to human activities Climate change will continue in the 21st century Warmer and drier conditions are expected, with more extreme events Significant impacts are likely Risk management requires consideration of low probability, high impact scenarios

  24. Thank you

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