Decadal Freshening and Warming of the Western Arctic Upper Ocean

Upper-ocean freshness and heat content are important components of the coupled Arctic system, especially within the context on ongoing Arctic change. High resolution hydrographic profile data collected from Arctic research expeditions and autonomous systems are analyzed to generate a 30+ year record...

Full description

Bibliographic Details
Main Author: Ingersoll, Russell G.
Other Authors: NAVAL POSTGRADUATE SCHOOL MONTEREY CA
Format: Text
Language:English
Published: 2010
Subjects:
Physical and Dynamic Oceanography
*ARCTIC OCEAN
*HEAT
*FRESH WATER
PERIODIC VARIATIONS
SALINITY
THESES
TEMPERATURE
MIXED LAYER(MARINE)
UPPER OCEAN
TRANS POLAR DRIFT
HEAT CONTENT
HALOCLINE
DEPARTURE FROM FREEZING POINT
CANADA BASIN
BEAUFORT GYRE
BEAUFORT SHELF
FRESH WATER CONTENT
Arctic
Arctic Ocean
Beaufort Shelf
Canada
canada basin
Sea ice
Online Access:http://www.dtic.mil/docs/citations/ADA531548
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA531548
Description
Summary:Upper-ocean freshness and heat content are important components of the coupled Arctic system, especially within the context on ongoing Arctic change. High resolution hydrographic profile data collected from Arctic research expeditions and autonomous systems are analyzed to generate a 30+ year record of upper-ocean fresh water content and heat content evolution. Vertical integrals of Heat Content (HC) and Fresh Water Content (FWC) are calculated in three layers: Surface(Sfc)-150m, Sfc-Mixed Layer Depth (MLD), and MLD-150m. Vertical averages of Departure From Freezing Point (DFFP), Salinity(z), and Temperature(z) are also calculated for all three layers. Spatial and temporal constraints allow for seasonal and regional signals to be separated from decadal trend signals. Sub-regions (Beaufort Shelf, Beaufort Gyre, and Trans-polar Drift) are chosen with respect to hydrographically uniform characteristics. In the Beaufort Gyre, Sfc-150m vertically averaged salinity decreases by -0.04 psu/yr while FWC increases by +0.15 m/yr, and HC rises by +3.8 MJ/sq m/yr. Mixed layer vs. Halocline trend separation (Sfc-MLD vs. MLD-150m) shows accumulation of FWC in both layers definitively, while the halocline hosts almost all of the accumulation of HC. The trends in FWC are consistent with the observed decline in Arctic sea ice cover. The original document contains color images.

Similar Items