scholarly journals Lidar-Derived Particle Concentrations in Plumes from Arctic Leads

1990 ◽  
Vol 14 ◽  
pp. 9-12 ◽  
Author(s):  
Edgar L. Andreas ◽  
Martin W. Miles ◽  
Roger G. Barry ◽  
Russell C. Schnell
Keyword(s):  
Arctic Ocean ◽  
Supercooled Water ◽  
Airborne Lidar ◽  
The Arctic ◽  
Water Droplets ◽  
Surface Source ◽  
The Arctic Ocean ◽  
Lidar Equation

With an airborne lidar, we have observed massive plumes of condensate particles rising from wintertime leads in the Arctic Ocean. Some of these plumes reached an altitude of 4 km; some extended over 200 km down-wind from their surface source. Here we invert the lidar equation and use lidar backscatter data to infer particle concentrations within two such plumes. Assuming that the plumes consist of supercooled water droplets of radius 5 μm, we estimate typical concentrations of 3–6 × 105 droplets m-3 just above the leads. Concentrations within the plumes can still be as high as 104 droplets m-3 at an altitude of 3 km and 200 km down-wind from some leads. Had we assumed that the plume particles are ice spheres of radius 40 μm, concentrations would be just 100 times less than these.

scholarly journals Lidar-Derived Particle Concentrations in Plumes from Arctic Leads

1990 ◽  
Vol 14 ◽  
pp. 9-12 ◽  
Author(s):  
Edgar L. Andreas ◽  
Martin W. Miles ◽  
Roger G. Barry ◽  
Russell C. Schnell
Keyword(s):  
Arctic Ocean ◽  
Supercooled Water ◽  
Airborne Lidar ◽  
The Arctic ◽  
Water Droplets ◽  
Surface Source ◽  
The Arctic Ocean ◽  
Lidar Equation

With an airborne lidar, we have observed massive plumes of condensate particles rising from wintertime leads in the Arctic Ocean. Some of these plumes reached an altitude of 4 km; some extended over 200 km down-wind from their surface source. Here we invert the lidar equation and use lidar backscatter data to infer particle concentrations within two such plumes. Assuming that the plumes consist of supercooled water droplets of radius 5 μm, we estimate typical concentrations of 3–6 × 105 droplets m-3 just above the leads. Concentrations within the plumes can still be as high as 104 droplets m-3 at an altitude of 3 km and 200 km down-wind from some leads. Had we assumed that the plume particles are ice spheres of radius 40 μm, concentrations would be just 100 times less than these.

scholarly journals Increasing coastal slump activity impacts the release of sediment and organic carbon into the Arctic Ocean

2018 ◽  
Vol 15 (5) ◽  
pp. 1483-1495 ◽  
Author(s):  
Justine L. Ramage ◽  
Anna M. Irrgang ◽  
Anne Morgenstern ◽  
Hugues Lantuit
Keyword(s):  
Organic Carbon ◽  
Arctic Ocean ◽  
Spline Interpolation ◽  
Airborne Lidar ◽  
Aerial Photographs ◽  
The Arctic ◽  
The Arctic Ocean ◽  
Arctic Coast ◽  
Coastal Retreat ◽  
High Resolution Satellite Imagery

Abstract. Retrogressive thaw slumps (RTSs) are among the most active thermokarst landforms in the Arctic and deliver a large amount of material to the Arctic Ocean. However, their contribution to the organic carbon (OC) budget is unknown. We provide the first estimate of the contribution of RTSs to the nearshore OC budget of the Yukon Coast, Canada, and describe the evolution of coastal RTSs between 1952 and 2011 in this area. We (1) describe the evolution of RTSs between 1952 and 2011; (2) calculate the volume of eroded material and stocks of OC mobilized through slumping, including soil organic carbon (SOC) and dissolved organic carbon (DOC); and (3) estimate the OC fluxes mobilized through slumping between 1972 and 2011. We identified RTSs using high-resolution satellite imagery from 2011 and geocoded aerial photographs from 1952 and 1972. To estimate the volume of eroded material, we applied spline interpolation on an airborne lidar dataset acquired in July 2013. We inferred the stocks of mobilized SOC and DOC from existing related literature. Our results show a 73 % increase in the number of RTSs and 14 % areal expansion between 1952 and 2011. In the study area, RTSs displaced at least 16.6×106 m3 of material, 53 % of which was ice, and mobilized 145.9×106 kg of OC. Between 1972 and 2011, 49 RTSs displaced 8.6×103 m3 yr−1 of material, adding 0.6 % to the OC flux released by coastal retreat along the Yukon Coast. Our results show that the contribution of RTSs to the nearshore OC budget is non-negligible and should be included when estimating the quantity of OC released from the Arctic coast to the ocean.

USGS Arctic Ocean Carbon Cruise 2012: Field Activity L-01-12-AR to collect carbon data in the Arctic Ocean, August-September 2012

Data Series ◽  
10.3133/ds862 ◽  
2014 ◽  
Author(s):  
Lisa L. Robbins ◽  
Jonathan Wynn ◽  
Paul O. Knorr ◽  
Bogdan Onac ◽  
John T. Lisle ◽  
...  
Keyword(s):  
Arctic Ocean ◽  
The Arctic ◽  
Field Activity ◽  
The Arctic Ocean ◽  
Ocean Carbon

A remarkable pogonophoran from a desalted shallow near the mouth of the Yenisey River in the Kara Sea, with the description of a new species of the genus Galathealinum (Annelida: Pogonophora: Frenulata)

2020 ◽  
Vol 29 (1) ◽  
pp. 138-154
Author(s):  
R.V. Smirnov ◽  
O.V. Zaitseva ◽  
A.A. Vedenin
Keyword(s):  
New Species ◽  
Arctic Ocean ◽  
Anterior Part ◽  
Morphological Characters ◽  
Kara Sea ◽  
The Arctic ◽  
External Layer ◽  
The Arctic Ocean ◽  
A New Species ◽  
Unusual Finding

A new species of Pogonophora obtained from one station at a depth of 25 m from near the Dikson Island in the Kara Sea is described. Galathealinum karaense sp. nov. is one of the largest pogonophorans, the first known representative of the rare genus Galathealinum Kirkegaard, 1956 in the Eurasian part of the Arctic Ocean and a highly unusual finding for the desalted shallow of the Yenisey Gulf. Several characters occurring in the new species are rare or unique among the congeners: under-developed, hardly discernible frills on the tube segments, extremely thin felted fibres in the external layer of the tube, and very faintly separated papillae in the anterior part of the trunk. Morphological characters useful in distinguishing species within the genus Galathealinum are defined and summarised in a table. Diagnosis of the genus Galathealinum is emended and supplemented by new characters. Additionally, three taxonomic keys are provided to the species of Galathealinum and to the known species of the Arctic pogonophorans using either animals or their empty tubes only, with the brief zoogeographical information on each Arctic species.

Positions of the non-Arctic States on the legal regime of the Arctic Ocean

2018 ◽  
pp. 124-135 ◽  
Author(s):  
A. Vylegzhanin ◽  
◽  
V. Salygin ◽  
I. Dudykina ◽  
E. Kienko ◽  
...  
Keyword(s):  
Arctic Ocean ◽  
The Arctic ◽  
Legal Regime ◽  
The Arctic Ocean
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