One More Step Toward a Warmer Arctic

Abstract

This study was motivated by a strong warming signal seen in mooring-based and oceanographic survey data collected in 2004 in the Eurasian% Basin of the Arctic Ocean. The source of this and earlier Arctic Ocean changes lies in interactions between polar and sub-polar basins. Evidence suggests such changes are abrupt, or pulse-like, taking the form of propagating anomalies that can be traced to higher-latitudes. For example, an anomaly found in 2004 in the eastern Eurasian Basin took 1.5 years to propagate from the Norwegian Sea to the Fram Strait region, and additional approx. 4.5-5 years to reach the Laptev Sea slope. While the causes of the observed changes will require further investigation, our conclusions are consistent with prevailing ideas suggesting the Arctic Ocean is in transition towards a new, warmer state.

Open PDF

Document Details

Document Type
Technical Report
Publication Date
Sep 09, 2005
Accession Number
ADA443077

Entities

People

  • Agnieszka Beszczynska
  • David Walsh
  • Eberhard Fahrbach
  • Eddy C. Carmack
  • Edmond Hansen
  • Igor A. Dmitrenko
  • Igor V. Polyakov
  • Ivan E. Frolov
  • Juergen Holfort
  • Ruediger Gerdes

Organizations

  • United States Naval Research Laboratory

Tags

Communities of Interest

  • C4I
  • Ground and Sea Platforms

DTIC Thesaurus Topics

  • Arctic Ocean
  • Atlantic Ocean
  • Boundaries
  • Canada
  • Climate
  • Heat Energy
  • Latitude
  • Military Research
  • North Atlantic Ocean
  • Norwegian Sea
  • Oceanography
  • Oceans
  • Physics Laboratories
  • Ridges
  • Sea Surface Temperature
  • Transitions
  • Universities

Fields of Study

  • Environmental science

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Oceanography.
  • Polar and Arctic Studies