TY - JOUR
T1 - Peculiarities of the formation of suspended particulate matter fields in the Eastern Arctic seas
AU - Charkin, A. N.
AU - Dudarev, Oleg Victorovich
AU - Shakhova, Natalia Evgenievna
AU - Semiletov, Igor Petrovich
AU - Pipko, Irina Ivanovna
AU - Pugach, Svetlana Petrovna
AU - Sergienko, V. I.
PY - 2015/6/29
Y1 - 2015/6/29
N2 - On the basis of perennial studies, the features of formations of suspended particulate matter fields were revealed depending on the evolution of synoptic processes and the river runoff. The variability in the content and distribution structure of suspended particulate matter during the ice-free period depends on variable mobilization and the contribution of terrigenous material under conditions of the Eastern Arctic periglacial lithogenesis. The northern winds and storms activate erosion of the coastal thermoabrasion benches and resuspension of sediments of the submarine coastal slope, resulting in an anomalous amount of suspended particulate matter in the coastal-shelf waters. Insignificant waves and dominant weak southern winds lead to other sedimentation conditions caused by suspended particulate matter accumulation.
AB - On the basis of perennial studies, the features of formations of suspended particulate matter fields were revealed depending on the evolution of synoptic processes and the river runoff. The variability in the content and distribution structure of suspended particulate matter during the ice-free period depends on variable mobilization and the contribution of terrigenous material under conditions of the Eastern Arctic periglacial lithogenesis. The northern winds and storms activate erosion of the coastal thermoabrasion benches and resuspension of sediments of the submarine coastal slope, resulting in an anomalous amount of suspended particulate matter in the coastal-shelf waters. Insignificant waves and dominant weak southern winds lead to other sedimentation conditions caused by suspended particulate matter accumulation.
UR - http://www.scopus.com/inward/record.url?scp=84938263081&partnerID=8YFLogxK
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U2 - 10.1134/S1028334X15060100
DO - 10.1134/S1028334X15060100
M3 - Article
AN - SCOPUS:84938263081
VL - 462
SP - 626
EP - 630
JO - Doklady Earth Sciences
JF - Doklady Earth Sciences
SN - 1028-334X
IS - 2
ER -