It is when you consider the performance of
water management systems, which have been built specifically for current
climatic conditions (Barnett et al., 2005).
A warmer climate would mean less snow accumulating during the winter period and
an earlier melt in the summer period. One region that climate change will have
a profound impact is in the Himalayan period, again as mentioned in previous
posts in terms of volume of ice, it has the 3rd largest in the
world, but what is crucial is that it supplies water to a significant part of
Asia. The China glacial inventory shows that there has been substantial melting
in most glaciers, one in particular has retreated 750 metres; alarming when it
is noted that it is the main contributor to the Yangtze river (Barnett et al., 2005). The inventory suggests
that the rate of glacial retreat is increasing.
To draw from another area of the world with
respect to proving glacial retreat is a real threat to societies we venture to
the Andes. The summit core of the Quelccaya glacier taken in 1976 was layered; it
showed the annual cycle of the glacier and could be traced back 1500 years. A
core was taken from the same glacier in 1991 and the layers from the past 20
years were non existent because of the percolation of meltwater (Barnett et al., 2005). Melting at the summit of the glacier is taking place and has been for the last 20 years, something that hasn’t happened in the previous 1500
years ago. Both examples show that glaciers are retreating and not just in one
area of the world….
My View
Clearly melting of glaciers is taking place, hopefully those reading this blog now realise this. Clearly it is going to have a high impact on the world and not just on one specific region but the impacts are likely to be felt in most areas of the world.
Clearly melting of glaciers is taking place, hopefully those reading this blog now realise this. Clearly it is going to have a high impact on the world and not just on one specific region but the impacts are likely to be felt in most areas of the world.
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