Little Fish, on 22 February 2013 - 06:31 PM, said:
AMO : Atlantic Multidecadel Oscillation :
now, what do you think the cause of arctic "ice loss" is?
and what do you think the future holds for the arctic ice given the above chart?
The problem is Little Fish that Arctic sea Ice and Glacial sea Ice are both lower than they have been in thousands of years and this doesn't fit at all with your cyclic AMO theory.
Let us also not forget that AMO is a climate response and not a driver.
Here's a graph which shows how poorly your AMO theory fits the known sea ice data;
http://en.wikipedia....0-part-2009.png
To put a more formal scientific slant on it;
Quote
Arctic sea-ice extent and volume are declining rapidly. Several studies project that the Arctic Ocean may
become seasonally ice-free by the year 2040 or even earlier. Putting this into perspective requires infor-
mationonthehistoryofArcticsea-iceconditionsthroughthegeologicpast.Thisinformationcanbeprovided
by proxyrecordsfrom the ArcticOcean floor and from the surroundingcoasts.Althoughexistingrecordsare
farfromcomplete,theyindicatethatseaicebecameafeatureoftheArcticby47 Ma,followingapronounced
decline in atmospheric pCO
2
after the Paleocene–Eocene Thermal Optimum, and consistently covered at
least part of the Arctic Ocean for no less than the last 13–14 million years. Ice was apparently most wide-
spread during the last 2–3 million years, in accordance with Earth’s overall cooler climate. Nevertheless,
episodes of considerably reduced sea ice or even seasonally ice-free conditions occurred during warmer
periods linked to orbital variations. The last low-ice event related to orbital forcing (high insolation) was in
theearlyHolocene,afterwhichthenorthernhighlatitudescooledoverall,withsomesuperimposedshorter-
term (multidecadal to millennial-scale) and lower-magnitude variability. The current reduction in Arctic ice
cover started in the late 19th century, consistent with the rapidly warming climate, and became very
pronounced over the last three decades. This ice loss appears to be unmatched over at least the last few
thousand years and unexplainable by any of the known natural variabilities.
Arctic paleoclimate proxies in lake and marine sediments, tree
rings, and ice cores indicate that from the mid-19th century the
Arctic not only warmed by more than 1
C average in comparison
with the ‘‘Little Ice Age’’ (
Overpecket al.,1997
), but also reached the
highest temperatures in at least the last two thousand years
(
Kaufman et al., 2009
). This warming sharply reversed the long-
term cooling trend that had likely been caused by the orbitally-
driven decreasing summer insolation with the positive feedbacks
from ice and snow albedo (e.g.,
Otto-Bliesner et al., 2006b
).
Subglacial material exposed by retreating glaciers in the Canadian
Arctic corroborates that modern temperatures are higher than any
time in at least the past 1600 years (
Anderson et al., 2008
). An even
longer perspective for the outstanding magnitude of the modern
warmingandrelatedicelossisprovidedbythehistoryoficeshelves
at the northern coast of Ellsemere Island, which are made of super-
thickened landfast ice supported by pack ice in the adjacent Arctic
Ocean.These ice shelves have been stable for most of the last5.5 kyr
basedondriftwoodages(
Englandetal.,2008
),butdeclinedbymore
than90%duringthe 20thcenturyandcontinuetobreakatanotable
rate (
Mueller et al., 2008
).
An unraveled magnitude and duration of modern sea-ice retreat
on a millennial background has been reported for the Nordic Seas
based on combined ice core and tree-ring proxy data from Svalbard
and Scandinavia (
Macias-Fauria et al., 2009
). A comparison of this
reconstruction with the Arctic-wide compilation of ice extent since
the mid-19th century (
Kinnard et al., 2008
) shows a close match
except for an obvious discrepancy in the early 20th century
(
Fig. 12
). This discrepancy reflects the pronounced warming event
in the Nordic Seas that was amplified by multidecadal variability of
the North Atlantic circulation (
Polyakov et al., 2009
) and therefore
affected primarily the Atlantic sector of the Arctic, somewhat
similar tothe 15th-century warming anomaly (
Crespin et al., 2009
).
In contrast, a very close match between the Nordic Seas and Arctic-
wide records of ice extent during the recent decades emphasizes
the pan-Arctic nature of the modern ice loss
http://www.geo.umass...R10 inpress.pdf
Far from the climate community denying the contribution of the AMO in causing changes in sea ice, they acknowledge it and account for it in their calculations of the current AGW induced decline.
Would you like a straw with your slushy sir
Br Cornelius
Edited by Br Cornelius, 23 February 2013 - 10:13 AM.
I believe nothing, but I have my suspicions.
Robert Anton Wilson