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Wednesday, May 31, 2017
RBI to introduce New Re.1 Note
The Reserve Bank of India has
announced that new one rupee note has been printed by the government and will
be soon put into circulation. The one rupee note was discontinued in 1994
because it was more expensive to produce such notes when compared to the
one-rupee coins. In the following year, Rs. 2 and Rs. 5 notes were also
discontinued to free up printing facilities for higher denomination notes.
However, these old notes continue to remain in circulation and continue to
remain as legal tenders. The new Re.1 one will be predominantly pink-green on
the obverse and reverse in combination with other colours. The new one rupee
note will bear the rupee symbol. It will be 9.7 by 8.3 cm in dimension. The new
note will feature ‘Bharat Sarkar’ on its masthead, and ‘Government of India’
printed below that. In contrast all the other currencies in India has
‘Bharatiya Reserve Bank’ and ‘Reserve Bank of India’ printed on them. This is
because the one-rupee note has always been issued by the central
government. The watermarks of the Re 1
note will include the Ashoka Pillar, the hidden numeral “1” and the hidden word
“Bharat” in Hindi). The note will also feature an image of the ‘Sagar Samrat’
oil exploration rig. In January 2015, the government began printing of Re 1
notes after getting reports of coin shortage along with instances of melting
coins for profit. The printing of new one rupee note will cost 94 paise, when
compared to the one rupee coin, which will cost 70 paise. The new one rupee
note will be the third new currency that will be introduced by the government
since the demonetization drive in November.
Tuesday, May 30, 2017
Anti-Ragging Mobile App Launched to Fight Ragging
Saturday, May 27, 2017
NASA Scientists Reveal a New Mode of Ice Loss in Greenland
A new NASA study published in
Geophysical Research Letters reveals that during Greenland’s hottest summers on
record, 2010 and 2012, the ice in Rink Glacier on the island’s west coast
didn’t just melt faster than usual, it slid through the glacier’s interior in a
gigantic wave, like a warmed freezer pop sliding out of its plastic casing. The
wave persisted for four months, with ice from upstream continuing to move down
to replace the missing mass for at least four more months.
This long pulse of mass loss,
called a solitary wave, is a new discovery that may increase the potential for
sustained ice loss in Greenland as the climate continues to warm, with
implications for the future rate of sea level rise.
The study by three scientists
from NASA’s Jet Propulsion Laboratory in Pasadena, California, was the first to
precisely track a glacier’s loss of mass from melting ice using the horizontal
motion of a GPS sensor. They used data from a single sensor in the Greenland
GPS Network (GNET), sited on bedrock next to Rink Glacier. A paper on the
research is published online in the journal Geophysical Research Letters.
Rink is one of Greenland’s major
outlets to the ocean, draining about 11 billion tons (gigatons) of ice per year
in the early 2000s — roughly the weight of 30,000 Empire State Buildings. In
the intensely hot summer of 2012, however, it lost an additional 6.7 gigatons
of mass in the form of a solitary wave. Previously observed melting processes
can’t explain that much mass loss.
The wave moved through the
flowing glacier during the months of June through September at a speed of about
2.5 miles (4 kilometers) a month for the first three months, increasing to 7.5
miles (12 kilometers) during September. The amount of mass in motion was 1.7
gigatons, plus or minus about half a gigaton, per month. Rink Glacier typically
flows at a speed of a mile or two (a few kilometers) a year.
The wave could not have been
detected by the usual methods of monitoring Greenland’s ice loss, such as
measuring the thinning of glaciers with airborne radar. “You could literally be
standing there and you would not see any indication of the wave,” said JPL
scientist Eric Larour, a coauthor of the new paper. “You would not see cracks
or other unique surface features.”
The researchers saw the same wave
pattern in the GPS data for 2010, the second hottest summer on record in
Greenland. Although they did not quantify the exact size and speed of the 2010
wave, the patterns of motion in the GPS data indicate that it must have been
smaller than the 2012 wave but similar in speed.
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