Abstract
A detailed analysis of dissolved organic carbon (DOC) distribution in the Western Arctic Ocean was performed during the spring and summer of 2002 and the summer of 2003. DOC concentrations were compared between the three cruises and with previously reported Arctic work. Concentrations of DOC were highest in the surface water where they also showed the highest degree of variability spatially, seasonally, and annually. Over the Canada Basin, DOC concentrations in the main water masses were: (1) surface layer (71±4 μM, ranging from 50 to 90 μM); (2) Bering Sea winter water (66±2 μM, ranging from 58 to 75 μM); (3) halocline layer (63±3 μM, ranging from 59 to 68 μM), (4) Atlantic layer (53±2 μM, ranging from 48 to 57 μM), and (5) deep Arctic layer (47±1 μM, ranging from 45 to 50 μM). In the upper 200 m, DOC concentrations were correlated with salinity, with higher DOC concentrations present in less-saline waters. This correlation indicates the strong influence that fluvial input from the Mackenzie and Yukon Rivers had on the DOC system in the upper layer of the Chukchi Sea and Bering Strait. Over the deep basin, there appeared to be a relationship between DOC in the upper 10 m and the degree of sea-ice melt water present. We found that sea-ice melt water dilutes the DOC signal in the surface waters, which is contrary to studies conducted in the central Arctic Ocean.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 3245-3258 |
| Number of pages | 14 |
| Journal | Deep-Sea Research Part II: Topical Studies in Oceanography |
| Volume | 52 |
| Issue number | 24-26 |
| DOIs | |
| State | Published - Dec 2005 |
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Keywords
- Arctic Ocean
- Carbon
- Chukchi Sea
- DOC
ASJC Scopus subject areas
- Aquatic Science
- Geology
- Oceanography
Cite this
Strong hydrographic controls on spatial and seasonal variability of dissolved organic carbon in the Chukchi Sea. / Mathis, Jeremy T.; Hansell, Dennis A; Bates, Nicholas R.
In: Deep-Sea Research Part II: Topical Studies in Oceanography, Vol. 52, No. 24-26, 12.2005, p. 3245-3258.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Strong hydrographic controls on spatial and seasonal variability of dissolved organic carbon in the Chukchi Sea
AU - Mathis, Jeremy T.
AU - Hansell, Dennis A
AU - Bates, Nicholas R.
PY - 2005/12
Y1 - 2005/12
N2 - A detailed analysis of dissolved organic carbon (DOC) distribution in the Western Arctic Ocean was performed during the spring and summer of 2002 and the summer of 2003. DOC concentrations were compared between the three cruises and with previously reported Arctic work. Concentrations of DOC were highest in the surface water where they also showed the highest degree of variability spatially, seasonally, and annually. Over the Canada Basin, DOC concentrations in the main water masses were: (1) surface layer (71±4 μM, ranging from 50 to 90 μM); (2) Bering Sea winter water (66±2 μM, ranging from 58 to 75 μM); (3) halocline layer (63±3 μM, ranging from 59 to 68 μM), (4) Atlantic layer (53±2 μM, ranging from 48 to 57 μM), and (5) deep Arctic layer (47±1 μM, ranging from 45 to 50 μM). In the upper 200 m, DOC concentrations were correlated with salinity, with higher DOC concentrations present in less-saline waters. This correlation indicates the strong influence that fluvial input from the Mackenzie and Yukon Rivers had on the DOC system in the upper layer of the Chukchi Sea and Bering Strait. Over the deep basin, there appeared to be a relationship between DOC in the upper 10 m and the degree of sea-ice melt water present. We found that sea-ice melt water dilutes the DOC signal in the surface waters, which is contrary to studies conducted in the central Arctic Ocean.
AB - A detailed analysis of dissolved organic carbon (DOC) distribution in the Western Arctic Ocean was performed during the spring and summer of 2002 and the summer of 2003. DOC concentrations were compared between the three cruises and with previously reported Arctic work. Concentrations of DOC were highest in the surface water where they also showed the highest degree of variability spatially, seasonally, and annually. Over the Canada Basin, DOC concentrations in the main water masses were: (1) surface layer (71±4 μM, ranging from 50 to 90 μM); (2) Bering Sea winter water (66±2 μM, ranging from 58 to 75 μM); (3) halocline layer (63±3 μM, ranging from 59 to 68 μM), (4) Atlantic layer (53±2 μM, ranging from 48 to 57 μM), and (5) deep Arctic layer (47±1 μM, ranging from 45 to 50 μM). In the upper 200 m, DOC concentrations were correlated with salinity, with higher DOC concentrations present in less-saline waters. This correlation indicates the strong influence that fluvial input from the Mackenzie and Yukon Rivers had on the DOC system in the upper layer of the Chukchi Sea and Bering Strait. Over the deep basin, there appeared to be a relationship between DOC in the upper 10 m and the degree of sea-ice melt water present. We found that sea-ice melt water dilutes the DOC signal in the surface waters, which is contrary to studies conducted in the central Arctic Ocean.
KW - Arctic Ocean
KW - Carbon
KW - Chukchi Sea
KW - DOC
UR - http://www.scopus.com/inward/record.url?scp=28844497407&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=28844497407&partnerID=8YFLogxK
U2 - 10.1016/j.dsr2.2005.10.002
DO - 10.1016/j.dsr2.2005.10.002
M3 - Article
AN - SCOPUS:28844497407
VL - 52
SP - 3245
EP - 3258
JO - Deep-Sea Research Part II: Topical Studies in Oceanography
JF - Deep-Sea Research Part II: Topical Studies in Oceanography
SN - 0967-0645
IS - 24-26
ER -