© 2013. American Geophysical Union. All Rights Reserved.
Eos, Vol. 94, No. 8, 19 February 2013
PAGE 76
August Arctic cyclone was strongest
summer storm on record
For nearly 2 weeks in August 2012, a
powerful cyclone churned the Arctic Ocean,
driving down surface pressures and garnering
significant public attention. Spawned over
Siberia on 2 August, the storm, which came to
be known as the “Great Arctic Cyclone of
2012,” died when it made landfall on the
shores of the Canadian High Arctic. Based on
observational records, researchers noted at
the time that the Great Arctic Cyclone had
the lowest sea surface pressure ever recorded
for an Arctic summer cyclone. Because the
storm coincided with what went on to
become the record‐breaking season for
minimum Arctic sea ice extent, some
researchers questioned whether the storm’s
severity may have been fueled by climate
change.
To identify the dynamics that may have
been responsible for the storm’s great strength
and longevity—and to determine whether the
August 2012 storm really lived up to its
moniker— Simmonds and Rudeva used a
cyclone analysis algorithm on the records of
the National Centers for Environmental
Prediction’s Climate Forecast System
Reanalysis.
Considering the storm’s central pressure,
intensity, radius, depth, and longevity, the
authors found that the August 2012 cyclone
was the strongest summer storm on record
and the 13th largest when the typically larger
winter cyclones were considered as well.
From 1979 to 2012, the length of the reanalysis
record, there were 19,625 cyclones. The
authors suggest that a tropopause polar
vortex, a persistent cyclonic rotation in the
upper atmosphere, that formed roughly
2 weeks before the onset of the Great Arctic
Cyclone contributed to the storm’s strength.
They add that rather than the cyclone being
fueled by reduced sea ice extent, the storm
instead spurred the ice’s decline. ( Geophysical
Research Letters, doi:10.1029/2012GL054259,
2012 ) —CS
New satellite record
of sea surface temperature
Sea surface temperature is one of the key
variables scientists track in studying climate
changes; it is also important to meteorology
and oceanography. Merchant et al . describe a
new 20‐year record of sea surface tempera-
ture. The record was created using infrared
imagery from the Along‐Track Scanning
Radiometers (ATSR) as part of the ATSR
Reprocessing for Climate (ARC) project.
The new record, the authors report, is more
accurate and stable than previous satellite‐
based sea surface temperature records. In
addition, the satellite measurements in the
new record are independent of in situ
measurements and thus provide a valuable
corroboration of the in situ record. The
authors believe the new data set will be
useful for quantifying interannual variability
in sea surface temperature as well as major
sea surface temperature anomalies. ( Journal
of Geophysical Research‐Oceans ,
doi:10.1029/2012JC008400, 2012) —EB
Io’s volcanism controls
Jupiter’s magnetospheric activity
Jupiter’s volcanic moon Io spews out
volcanic gas, which reaches its atmosphere
and becomes ionized, forming what is
known as the Io plasma torus. This plasma
torus can interact with Jupiter’s magneto-
sphere, possibly affecting auroral activity
there. To help determine whether Io’s
volcanic activity affects Jupiter’s magneto-
sphere, Yoneda et al . analyzed ground‐based
observations of Jupiter’s sodium nebula,
which provides an indication of Io’s volcanic
activity and plasma content in the Io plasma
torus, along with satellite‐based measure-
ments of the radio emission called hectomet-
ric (HOM) emission, which is a sign of
Jupiter’s auroral activity.
The researchers observed that Jupiter’s
sodium nebula was enhanced in late May
through early June 2007, indicating that Io’s
volcanic activity increased during that period.
They observed that shortly after this enhance-
ment began, Jupiter’s HOM emission intensity
decreased. As a result, the authors conclude
that increased volcanic activity on Io lessens
auroral activity in Jupiter’s magnetosphere.
( Geophysical Research Letters , doi:10.1002/
grl.50095, 2013) —EB
Seabirds influence Arctic methane
and nitrous oxide emissions
Seabird activity is contributing significantly
to methane and nitrous oxide emissions in
the Arctic tundra, a new study shows.
Methane emissions, which play an important
role in the global carbon cycle, and nitrous
oxide fluxes, a key element in the nutrient
cycle, are predicted to increase in the Arctic
and contribute to Arctic warming in the
near future.
To study the effects of seabird activity on
variations in nitrous oxide and methane fluxes
from the tundra to the atmosphere, Zhu et al .
compared fluxes from a seabird sanctuary
and two non‐seabird colonies on Ny‐Ålesund,
Svalbard, Norway. They found that seabird
activity was a major factor in these emissions.
Mean fluxes of nitrous oxide were about
18 micrograms per square meter per hour at
the seabird sites, compared with about
8 micrograms per square meter per hour at the
tundra sites without seabirds. For methane,
seabird activity actually changed the tundra
from a methane sink to a source: mean fluxes
of methane were about 53 micrograms per
square meter per hour at the seabird sites and
about ‐83 micrograms per square meter per
hour at the sites without seabirds.
The researchers considered other factors
that could influence methane and nitrous
oxide emissions, including soil moisture and
temperature. However, they found that
seabird activity was the predominant factor in
controlling the flux of these gases from the
tundra to the atmosphere. They concluded
that sites with high seabird activity are likely
to be hotspots of methane and nitrous oxide
emissions. ( Journal of Geophysical Research‐
Biogeosciences , doi:10.1029/2012JG002130,
2012) —EB
— ERNIE BALCERAK , Staff Writer, and
COLIN SCHULTZ, Writer
Average distribution of sea surface temperature in the month of October, from 20 years of satellite data. R
enbi
n Zh
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A seabird sanctuary, located at Ny-Ålesund (78° 55′′N, 11° 56′E) on the western coast of Spitsbergen, Svalbard, in the High Arctic region. In this sanctuary, the active main species of seabirds include Arctic duck, razor-billed auk, and kittiwake.