ICEandSNOW final compressed

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Slide1: 

United Nations Environment Programme - 2007

Components of the Cryosphere: 

Introduction Snow Ice in the sea Ice on land huge ice sheets, and the smaller glaciers and ice caps Frozen ground River and lake ice Components of the Cryosphere

Why are Ice and Snow Important to Us?: 

Ice and snow are important in many regions of the world for biodiversity, water supplies, livelihoods, culture, recreation… because they influence flood risk, construction, transportation, agriculture, resource extraction… Why are Ice and Snow Important to Us? Armin Rose/iStockphoto.com

Why are Ice and Snow Important to Us?: 

Ice and snow are important factors in global processes Climate Carbon balance Sea level Why are Ice and Snow Important to Us?

Why are Ice and Snow Important to Us?: 

Ice and snow affect the global distribution of heat Ocean currents distribute heat: thermohaline circulation depends on deep, cold water formed in the polar regions. Melting ice weakens this process. Why are Ice and Snow Important to Us?

Slide6: 

The bright surface of ice and snow cover reflects sunlight and cools the planet. Warmer temperatures More sunlight absorbed by land and sea Less ice and snow Melting of ice and snow speeds up global warming (positive feedback). Positive feedback of melting ice and snow

Why are Ice and Snow Changing?: 

Temperatures are rising. Natural variability influences climate - but most of the recent warming is very likely due to increased greenhouse gas emissions. Why are Ice and Snow Changing?

Slide8: 

The Arctic is warming at almost twice the rate of the rest of the world. In many areas the mountains are warming faster than the lowlands. 2001-2005 temperatures compared with the 1951-1980 mean.

Slide9: 

During the 21st century, increases in greenhouse gas emissions will be the most important external influence on ice and snow. Ian Britton/FreeFoto.com

Slide10: 

Artis Rams/iStock Snow influences climate because of its insulating properties and because it reflects sunlight. Less snow leads to acceleration of global warming Snow

Snow: trends: 

Snow cover has declined in the Northern Hemisphere, especially in spring and summer. Mean monthly snow cover is decreasing by about 1.3% per decade. Snow: trends

Snow: outlook: 

Snow: outlook Yellow to red is less snow Blue is increased snow The snow line is projected to rise in many mountain areas Major reductions in snow cover are projected for mid-latitudes by the end of the 21st century.

Slide13: 

Snow: impacts Changes in snow cover have a dramatic impact on water resources. Snow in mountain regions contributes to water supplies for almost one-sixth of the world’s population. Snow is an important ecological factor and changes in snow affect plants and animals Peter Prokosch

Slide14: 

Snow: impacts Changes in snow affect reindeer and caribou and the Arctic indigenous people who depend upon them. Inger Marie Gaup Eira/www.ealat.org Arctic ecosystems

Slide15: 

Snow: impacts Each degree warmer in the winter means poor snow conditions for more ski resorts. Many will be forced to shut down. Winter recreation

Slide16: 

Jon Aars/NPI Sea ice influences climate because it reflects sunlight and because it influences ocean circulation. Less sea ice leads to acceleration of global warming Ice in the Sea

Slide17: 

Sea Ice: trends Arctic sea-ice cover is shrinking by 8.9% per decade in summer and 2.5% per decade in winter. It is also becoming thinner and there is less multi-year ice. Antarctic sea-ice cover is not decreasing.

Slide18: 

Sea Ice: outlook Arctic sea-ice extent and thickness are projected to decline with a possibility of a mainly ice-free Arctic Ocean in summer by 2100 or earlier. Antarctic sea ice is also projected to decline in this century. Mlenny/iStock

Slide19: 

Sea Ice: impacts Melting sea ice, in combination with melting glaciers and ice sheets, may cause major changes to global patterns of ocean circulation. As with snow, less sea ice increases absorption of heat from the sun, resulting in increased warming Don Perovich

Slide20: 

Sea Ice: impacts Sea ice is habitat for many organisms – from bacteria, algae, sea worms and crustaceans to sea birds, penguins, seals, walrus, polar bears and whales. Photos: (1,2) Håkon Hop/NPI, (3)www.glaciers-online.net

Slide21: 

Sea Ice: impacts Some sea-ice dependent animals are already at risk and the predicted declines in sea ice may lead to extinctions. Photos: (1) Jon Aars/NPI, (2) Georg Bangiord

Slide22: 

Sea Ice: impacts Shrinking sea ice is affecting Arctic indigenous people and further loss of sea ice threatens livelihoods and cultures. Bjørn Frantzen

Slide23: 

Sea Ice: impacts More open water in polar regions will provide easier access to oil and gas reserves and increase shipping and tourism, with accompanying benefits and risks.

Slide24: 

Greenland and Antarctica contain about 99% of the freshwater ice on Earth’s surface. Meltwater from ice sheets contributes to sea level rise. Konrad Steffen Ice Sheets

Slide25: 

Ice on land Annual total loss of mass from the Greenland Ice Sheet more than doubled in the last decade of the 20th century and may have doubled again by 2005. Warmer summers are increasing melting and ice discharge. Greenland: recent changes Yellow = no or little change Blue = snow accumulation Red = less mass (melting and discharge of ice) Ice Sheets: trends

Slide26: 

Yellow = no or little change Blue = snow accumulation Red = less mass (melting and discharge of ice) Ice Sheets: trends Antarctica: recent changes There is uncertainty concerning recent overall changes in ice mass in the Antarctic Ice Sheet, but there is probably a decline in mass. Ice shelves are thinning and some are breaking up.

Slide27: 

Ice Sheets: trends Surprising changes that models cannot simulate, including thinning of outlet glaciers and ice shelves, have been observed over the past five years. NSIDC Break-up of the Larsen B Ice Shelf, 2002

Slide28: 

Recent signs point to accelerating loss of ice in both Greenland and Antarctica. Some of these changes are not caused by melting but by changes in glacier dynamics and are poorly understood. Ice Sheets: outlook Because of this it is not possible to predict the future of the ice sheets with any confidence. Konrad Steffen

Slide29: 

Glaciers and ice caps are important freshwater resources, but also natural hazards. Glaciers are close to the melting point and react strongly to climate change. Igor Smichkov/iStock Glaciers and Ice Caps

Slide30: 

Glaciers: trends Over the past 100 years, and particularly since the 1980s, there has been worldwide and dramatic shrinking of glaciers, closely related to global warming. Jürg Alean, SwissEduc (www.swisseduc.ch)/Glaciers online (www.glaciers-online.net)

Slide31: 

Glaciers: outlook 2006 1976 1933 Fedchenko Glacier, Tajikistan V.Novikov Projected increases in global air temperatures will ensure the continuing shrinkage of glaciers and may lead to their disappearance from many mountain regions in the coming decades.

Slide32: 

Glaciers: impacts Disappearance of glaciers will have major consequences on water resources, especially in the Himalayas – Hindu Kush, the Andes, Rocky Mountains and European Alps. Himalayas – Hindu Kush: major rivers draining glaciers and populations in their basins

Slide33: 

Glaciers: impacts Shrinkage of glaciers leads to ice instability and formation of ice and debris dams, resulting in more flooding, debris flows and ice avalanches. Ice avalanches of the Nevados Huascarán in Peru.

Slide34: 

Meltwater from ice sheets, glaciers and ice caps contribute to sea-level rise. How much the sea level rises relative to the adjacent coast varies from place to place. Bruce Richmond/USGS Sea-level Change

Slide35: 

Sea Level Rise: trends Sea level is rising now by 3.1 mm per year, double the average rate of the 20th century.

Slide36: 

Sea Level Rise: outlook The contribution from meltwater to sea level rise can be expected to accelerate as more land ice melts. In the long run, the ice sheets have the potential to make the largest contribution to sea-level rise. Contributions to sea-level rise Greenland Ice Sheet

Slide37: 

Sea Level Rise: outlook For the next few decades the rate of sea-level rise is partly locked in by past emissions. Sea-level in the late 21st century and beyond is critically dependent on future greenhouse gas emissions. Bruce Miller IPCC projections are for a global sea level rise of 20 to 80 cm over the 21st century. The upper bound is very uncertain.

Slide38: 

Sea Level Rise: impacts The impacts of sea-level rise in any region will depend on many interacting factors, such as whether the coastal region is undergoing uplift or subsidence; how much development has altered natural flood protection, like coastal vegetation. Bangladesh is made more vulnerable to flooding by the expansion of aquaculture which results in loss of mangroves. A sea-level rise of 20 to 40 cm will drastically reduce the number of annual rice crops in the Mekong delta. Island tourism in Malaysia is expected to be compromised by rising sea level because of beach erosion and salt contamination of water supplies.

Slide39: 

Sea Level Rise: impacts Magnitude of the issue Rising sea levels, combined with increased extreme events, will potentially affect millions of people on small islands and at and near coasts world-wide. Asia: a one metre sea-level rise would affect Land: 900,000 km2 People: over 100 million Economic activity: over US$400 billion in GDP Veer

Slide40: 

Sea Level Rise: adaptation and mitigation A wide range of adaptation and mitigation measures will be required to assist people with the consequences of sea-level rise. These measures require cooperation among nations, and among governments, private sector, researchers, NGOs and communities Restoring shoreline vegetation, Fiji Patrick Nunn

Slide41: 

Sea Level Rise: adaptation Adaptation Strategies: Accommodation: increase resilience, for example through providing storm shelters and warning systems Protection: such as barriers, dykes and vegetation Planned retreat: for example, designate no-build areas or setbacks from coasts The Environment Agency Patrick Nunn Thames Barrier, London Kiribati

Slide42: 

Permafrost occupies up to 24% of land in the Northern Hemisphere. Permafrost is also under parts of polar seas, in mountain regions and Antarctica. Vladimir Romanovsky Frozen Ground

Slide43: 

Permafrost: trends Permafrost temperatures have increased during the last 20-30 years in almost all areas of the Northern Hemisphere. Warming is reported from areas of mountain permafrost. Widespread thawing is not yet occurring. Dark blue is continuous permafrost Permafrost in the Northern Hemisphere

Slide44: 

Permafrost: outlook Dark red is zones of thawing permafrost Projected changes in permafrost temperatures by 2080 - 2099 Permafrost thawing is expected to occur across the subarctic by the end of the 21st century.

Slide45: 

Frozen ground Permafrost: impacts When permafrost thaws carbon is released in the form of greenhouse gases, accelerating global warming. Thawing of ice-rich permafrost results in the land surface subsiding. On a large scale, permafrost thawing changes ecosystems – for example, changing forest to wetland.

Slide46: 

Construction and everyday use of permafrost can result in permafrost thawing – damaging the infrastructure. Warming may accelerate this. Good engineering practices prevent permafrost thawing. Permafrost: impacts Roger Asbury/iStock Photo

Slide47: 

In mountainous areas, thawing permafrost increases risk of landslides and rock falls and has impacts on infrastructure. Permafrost in China has degraded over the past 40 years and is projected to decrease by 30-50% in this century. Permafrost: impacts S. Marchenko

Slide48: 

Floating freshwater ice is a key component of cold-regions river and lake systems, mainly in the Northern Hemisphere and mountain regions. River and Lake Ice Esko Kuusisto

Slide49: 

R. Borgström River and Lake Ice: trends Changes that have largely mirrored rising air temperatures are affecting river and lake ice. Main change is earlier spring break up and, to a lesser degree, later autumn freeze up.

Slide50: 

River and Lake Ice: outlook R. Borgström The trend to longer ice-free periods is projected to continue, with the amount of change projected for each region being related to the amount of warming forecast.

Slide51: 

River and Lake Ice: impacts In remote areas frozen rivers and lakes are used as transport corridors and longer ice-free periods mean reduced or more expensive access to communities and industrial developments. T.D. Prowse

Slide52: 

River and Lake Ice: impacts Many northern indigenous people depend on frozen lakes and rivers for access to traditional hunting, fishing, reindeer herding or trapping areas. Shari Gearheard

Slide53: 

River and Lake Ice: impacts Spring break up often causes damming of rivers by ice, resulting in costly flooding. Lowered temperature gradients on northward-flowing Northern Hemisphere rivers may result in reduced flooding. This has potential negative ecological consequences where annual flooding maintains important wetlands. Dörte Köster

Slide54: 

The underlying theme of the Global Outlook for Ice and Snow is that changes are now observed in ice and snow and bigger changes are projected. This raises policy issues at global, regional and local scales. Christian Lambrechts Policy and Perspectives

Slide55: 

Mitigating climate change by reducing greenhouse gas emissions is the main global policy response. IPCC 4th Assessment: to avoid further and accelerated global warming with major negative consequences, greenhouse gases must stop increasing and start decreasing no later than 15 to 25 years from now. Policy: global

Slide56: 

Adaptation policy must be tailored to regions and this requires regional scientific knowledge and impact assessment. Arctic: key policy issues: retreating sea ice and implications for shipping and exploitation of oil and gas reserves, accompanied by issues of jurisdiction and regulation for environmental protection. Policy: regional A. Taurisano/NPI

Slide57: 

Antarctic: a key policy issue: decreasing sea ice could contribute to rapid expansion of tourism industry: potential negative impacts and need for regulatory regime. Policy: regional

Slide58: 

Policy: regional Himalayas – Hindu Kush: a key policy focus: changes in snowfall and glaciers potentially increasing floods and leading to water shortages affecting hundreds of millions of people: strategies for water management and land use planning to reduce vulnerability. Falk Kienas/iStock

Slide59: 

Policy: local Impacts of changes in ice and snow are already major concerns in many Arctic communities. Issues include erosion of coastal infrastructure and access to subsistence resources. Expansion of shipping and oil and gas development will bring both local opportunities and potential negative economic and social effects. Most Arctic communities lack capacity to cope effectively with these stresses. Stine Rybråten

Slide60: 

Perspectives

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