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Hubbard Glacier Global warming Ice calving Retreat of glaciers since 1850
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Series of 5 sequential images showing Ice calving from Hubbard Glacier, Alaska 4/5
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Global warming

Global warming refers to the rising average temperature of Earth's atmosphere and oceans and its projected continuation. In the last 100 years, Earth's average surface temperature increased by about 0.8 °C (1.4 °F) with about two thirds of the increase occurring over just the last three decades. Warming of the climate system is unequivocal, and scientists are more than 90% certain most of it is caused by increasing concentrations of greenhouse gases produced by human activities such as deforestation and burning fossil fuels. These findings are recognized by the national science academies of all the major industrialized countries.

Climate model projections are summarized in the 2007 Fourth Assessment Report (AR4) by the Intergovernmental Panel on Climate Change (IPCC). They indicate that during the 21st century the global surface temperature is likely to rise a further 1.1 to 2.9 °C (2 to 5.2 °F) for their lowest emissions scenario and 2.4 to 6.4 °C (4.3 to 11.5 °F) for their highest. The ranges of these estimates arise from the use of models with differing sensitivity to greenhouse gas concentrations.

An increase in global temperature will cause sea levels to rise and will change the amount and pattern of precipitation, and a probable expansion of subtropical deserts. Warming is expected to be strongest in the Arctic and would be associated with continuing retreat of glaciers, permafrost and sea ice. Other likely effects of the warming include more frequent occurrence of extreme weather events including heat waves, droughts and heavy rainfall events, species extinctions due to shifting temperature regimes, and changes in crop yields. Warming and related changes will vary from region to region around the globe, with projections being more robust in some areas than others. In a 4 °C world, the limits for human adaptation are likely to be exceeded in many parts of the world, while the limits for adaptation for natural systems would largely be exceeded throughout the world. Hence, the ecosystem services upon which human livelihoods depend would not be preserved.

TEXT FROM WIKIPEDIA, cba SOME RIGHTS RESERVED.
Hubbard Glacier

Hubbard Glacier is a glacier located in eastern Alaska and part of Canada.

The longest source for Hubbard Glacier originates 122 kilometres (76 mi) from its snout and is located at about at about 61°00′N 140°09′W / 61°N 140.15°W / 61; -140.15, approximately 8 kilometres (5.0 mi) west of Mt. Walsh with an altitude around 11,000 feet (3,400 m). A shorter tributary glacier begins at the easternmost summit on the Mt. Logan ridge at about 18,300 feet (5,600 m) at about 60°35′0″N 140°22′40″W / 60.583333°N 140.37778°W / 60.583333; -140.37778.

Before it reaches the sea, Hubbard is joined by the Valerie Glacier to the west, which, through forward surges of its own ice, has contributed to the advance of the ice flow that experts believe will eventually dam the Russell Fiord from Disenchantment Bay waters.

The Hubbard Glacier ice margin has continued to advance for about a century. In May 1986, the Hubbard Glacier surged forward, blocking the outlet of Russell Fjord and creating "Russell Lake." All that summer the new lake filled with runoff; its water level rose 25 metres (82 ft), and the decrease in salinity threatened its sea life.

TEXT FROM WIKIPEDIA, cba SOME RIGHTS RESERVED.
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