Did you know?
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The Gangotri glacier is retreating at a speed of about 30 metres a
year and warming is likely
to increase the rate of melting |
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The Gangotri glacier in the
Himalayas is the source of water for the perennial river Ganga. This glacier like many
others all over the world has also felt the impact of climate change. Studies carried out
in the past few years have shown that the glacier is retreating at a speed of about 30
metres every year. If warming continues, it will melt rapidly, releasing large volumes of
water but once this source begins drying, there may be dry periods with very little water
flowing in the river. Source
IPCC Third Assessment Report. 2001
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| A 1-metre rise in sea level would displace about 7 million people
in India |
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If the earth's surface warms by
about 2 ºC, sea levels are expected to rise because of two factors: first, glaciers and
polar ice sheets will melt and release water into the seas and oceans. Second, water will
expand due to heating and also contribute to a rise in sea level. By 2100, a rise of about
9 cm to 88 cm is expected which will have a physical impact on coastal areas by increasing
flooding and the intrusion of salt water. Low-lying areas of the world may be submerged
leaving the people who live there homeless and landless. In the developing countries and
small island states, coastal areas are densely populated and millions of people are likely
to be affected - about 7 million people in our own country are projected to suffer the
effects of a 1-m sea-level rise. Source
IPCC Third Assessment Report. 2001
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| Fossil-fuel burning has contributed to most of the greenhouse gas
emissions in the past 20 years |
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About three-quarters of the
anthropogenic emissions of carbon dioxide to the atmosphere during the past 20 years have
been due to fossil-fuel burning. Activities consuming fossil fuels include power
generation, industrial/manufacturing processes, transport. The rest of carbon dioxide
emissions are predominantly due to land-use change, especially deforestation. Source
IPCC Third Assessment Report. 2001
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| The decade of the 1990s was the warmest, and 1998 was the warmest
year on record, since 1861 |
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Scientists began systematically
recording temperatures at specific locations on the earth's surface around the 1860s.
Since then, 1998 has been the hottest year and the decade of the 1990s was the warmest.
The increase in surface temperature over the 20th century for the Northern Hemisphere is
likely to have been greater than for any other century in the last thousand years. Source IPCC Third Assessment
Report. 2001
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| The population of ice-dependent penguin species in the Western
Antarctic Peninsula has decreased by 20% over the last 25 years |
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In the Western Antarctic
Peninsula, there has been a 20% decrease in the number of Adelie penguins since 1973
because sea ice is melting and reducing their habitat. Evidence from marine ecosystems has
shown changes in the abundance of species, diversity and spatial distribution associated
with rises in the air and ocean temperature. Decreases in the population of Adelie (Pygoscelis
adeliae) penguins, and declines in rockhopper penguins in recent decades could have
also been caused by differential responses to warming climate conditions that are altering
bird habitats. Researchers think that higher temperatures may have melted ice shelves,
which in turn, cooled the surrounding sea water unusually. This could have affected the
entire food chain, reducing the amount of food available to the penguins. Source IPCC Third Assessment
Report. 2001
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| Projections for the 21st century indicate that the earth's average
temperature will rise by anything between 1.4 and 5.8ºC |
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The global-average surface
temperature is projected to increase by 1.4 to 5.8°C over the period 1990 to 2100. There
is a range associated with these temperature projections because they are based on
different scenarios. These scenarios assume different social, technological, economic, and
demographic levels of development, so the projected concentrations of GHGs under each
scenario also vary. There are other uncertainties due to the effects of climate feedback
and carbon sinks (removal processes). Source
IPCC Third Assessment Report. 2001 |