Table of contents
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Part A
What is up for discussion?

Hot Issue in Cold Environment! How can it serve Climate?
Introduction
(A) A climatic revolution
(B) Objective of investigation
(C) Where, When, Why

Part B
Warming of Spitsbergen, Facts and Considerations

Use of temperature series
What offers modern science?
How the warming was discussed until the 1940s
 

Part C
Analysing the warming event

General observations
Which sea areas could have contributed?
The warming event in detail
  1. Exceptional temperatures
  2. Distant warming
  3. Arctic Ocean
  4. Greenland
  5. Barents Sea
  6. Europe
  7. Is Spitsbergen the sole heating-up spot?
 

Part D
What caused the Arctic-warming?

What does not explain the warming?
Ocean’s potential – Ocean’s forcing
Which causing mechanism should be discussed?
Can WWI have caused the Spitsbergen warming?
(A) Which potential forces are available?
(B) Naval force a force to recon
  1. Why naval force?
  2. How close was the naval war to Spitsbergen?
  3. When got naval war in full swing?
  4. Weapon scenario that stirred the seas
  5. Churning the sea activities.
  6. Other means causing alterations
(C) Linking Naval war to Arctic-warming
  1. The general situation
  2. The week point of linking the events
  3. A further strong point of linking the events
(D) Conclusion
 
Annexes
Annex A - Spitsbergen Temp Birkeland
Annex B - Original Sea Ice graphs 1910-1919
Annex C - Colored Sea Ice graphs 1910-1919
Annex D - Winter weather conditions 1916 - 1917
Annex E - Winter weather conditions 1916 - 1918

Last revised October 2007. All information and figures are by approximation, and may be altered and changed without notice.


29 April 2008

Catherine Brahic on:
Arctic currents may be warming the world

In: New Scientist -26 April 2008, Magazine issue 2653

THERE may be more to global warming than we thought. On top of the effect of human-made carbon emissions, natural changes in the warm ocean currents travelling to the icy north may be helping to heat up the entire northern hemisphere.
Temperatures in the Arctic are rising far faster than in other parts of the world. Climate models produced by the Intergovernmental Panel on Climate Change (IPCC), which are tuned to reproduce the human-made greenhouse effect, predict the region should have warmed by 1.4 °C between 1960 and 2000. In fact, the Arctic's average air temperature rose by 2.2 °C.
Vladimir Semenov of the Obukhov Institute of Atmospheric Physics in Moscow, Russia, says that ocean currents carrying warm water from lower latitudes into polar regions could have played a part in this increase.
Text from: http://environment.newscientist.co

This website has more to tell about the arctic warming issue. It deals comprehensively with the much more pronounced arctic warming that started 90 years ago at the remote Archipelagos of Spitsbergen at latitude 78 degrees North. It assesses in detail what Vladimir Semenov (see the box) and his colleagues had to say about the earlier warming in 2004[1]; see: Chapter B, “What offers modern science”. Although they acknowledge that: “The huge warming of the Arctic, which started in the early 1920s and lasted for almost two decades (see graph below), is one of the most spectacular climate events of the 20th century”, this website is giving you a more in-depth research on what happened back in the late 1910s with many references and graphs. As necessary as it is to investigate and discuss the situation in the Arctic and its global warming potential, one will remain in the dark as long as the early arctic warming is not fully explained and understood, to which this website wants to be a service, and you can find out whether it is. Have an interesting reading,
wishes the Arctic-warming-team

 

[1] Lennart Bengtsson • Vladimir A. Semenov • Ola Johannessen, The early century warming in the Arctic – A possible mechanism, 2003, Report No. 345, Max-Planck-Institute of Meteorology, Hamburg, Germany;
ditto at:  Journal of Climate, October 2004, page 4045-4057

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Related sites
 

PACON 2007, 20th Conference:
Ocean Observing Systems and Marine Environment
Honolulu, Hawaii, June 24-27

 

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Pages: 325-337.
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