Standard

Lena Delta hydrology and geochemistry. / Fedorova, I.; Chetverova, A.; Bolshiyanov, D.; Makarov, A.; Boike, J.; Heim, B.; Morgenstern, A.; Overduin, P.; Wegner, C.; Kashina, V.; Eulenburg, A.; Dobrotina, E.; Sidorina, I.

In: Biogeosciences Discussions, Vol. 10, 23.12.2013, p. 20179-20237.

Research output: Contribution to journal › Article › peer-review

Harvard

Fedorova, I, Chetverova, A, Bolshiyanov, D, Makarov, A, Boike, J, Heim, B, Morgenstern, A, Overduin, P, Wegner, C, Kashina, V, Eulenburg, A, Dobrotina, E & Sidorina, I 2013, 'Lena Delta hydrology and geochemistry', Biogeosciences Discussions, vol. 10, pp. 20179-20237. https://doi.org/10.5194/bgd-10-20179-2013

APA

Fedorova, I., Chetverova, A., Bolshiyanov, D., Makarov, A., Boike, J., Heim, B., Morgenstern, A., Overduin, P., Wegner, C., Kashina, V., Eulenburg, A., Dobrotina, E., & Sidorina, I. (2013). Lena Delta hydrology and geochemistry. Biogeosciences Discussions, 10, 20179-20237. https://doi.org/10.5194/bgd-10-20179-2013

Vancouver

Fedorova I, Chetverova A, Bolshiyanov D, Makarov A, Boike J, Heim B et al. Lena Delta hydrology and geochemistry. Biogeosciences Discussions. 2013 Dec 23;10:20179-20237. https://doi.org/10.5194/bgd-10-20179-2013

Author

Fedorova, I. ; Chetverova, A. ; Bolshiyanov, D. ; Makarov, A. ; Boike, J. ; Heim, B. ; Morgenstern, A. ; Overduin, P. ; Wegner, C. ; Kashina, V. ; Eulenburg, A. ; Dobrotina, E. ; Sidorina, I. / Lena Delta hydrology and geochemistry. In: Biogeosciences Discussions. 2013 ; Vol. 10. pp. 20179-20237.

BibTeX

@article{21b063ab246644d4bbbe4115e14d966e,
title = "Lena Delta hydrology and geochemistry",
abstract = "The Lena River forms one of the largest deltas in the Arctic; studying this delta has raised many questions regarding processes that occur there that remain open today. Comparing long-term hydrometric observational data of Russian Federal Service for Hydrometeorology and Environmental Monitoring (Roshydromet) from the Khabarova polar station, located at the head of the delta not far from where the Lena River divides into its main branches, with field observations, which have been carried out since 2002 revealed new insights into the hydrological, hydrochemical, and geochemical processes within the delta. Three periods with various water volumes and intensity of fluvial processes were chosen from the long-term record of water and sediment discharge. The role of ice event (ice blockage and ice floating) during high water in reconfiguring branch channels and influencing the volume of sediment runoff was identified. Results were obtained quantifying the increase of water and sediment discharges in the middle part",
author = "I. Fedorova and A. Chetverova and D. Bolshiyanov and A. Makarov and J. Boike and B. Heim and A. Morgenstern and P. Overduin and C. Wegner and V. Kashina and A. Eulenburg and E. Dobrotina and I. Sidorina",
year = "2013",
month = dec,
day = "23",
doi = "10.5194/bgd-10-20179-2013",
language = "English",
volume = "10",
pages = "20179--20237",
journal = "Biogeosciences Discussions",
issn = "1810-6277",
publisher = "European Geosciences Union",

}

RIS

TY - JOUR

T1 - Lena Delta hydrology and geochemistry

AU - Fedorova, I.

AU - Chetverova, A.

AU - Bolshiyanov, D.

AU - Makarov, A.

AU - Boike, J.

AU - Heim, B.

AU - Morgenstern, A.

AU - Overduin, P.

AU - Wegner, C.

AU - Kashina, V.

AU - Eulenburg, A.

AU - Dobrotina, E.

AU - Sidorina, I.

PY - 2013/12/23

Y1 - 2013/12/23

N2 - The Lena River forms one of the largest deltas in the Arctic; studying this delta has raised many questions regarding processes that occur there that remain open today. Comparing long-term hydrometric observational data of Russian Federal Service for Hydrometeorology and Environmental Monitoring (Roshydromet) from the Khabarova polar station, located at the head of the delta not far from where the Lena River divides into its main branches, with field observations, which have been carried out since 2002 revealed new insights into the hydrological, hydrochemical, and geochemical processes within the delta. Three periods with various water volumes and intensity of fluvial processes were chosen from the long-term record of water and sediment discharge. The role of ice event (ice blockage and ice floating) during high water in reconfiguring branch channels and influencing the volume of sediment runoff was identified. Results were obtained quantifying the increase of water and sediment discharges in the middle part

AB - The Lena River forms one of the largest deltas in the Arctic; studying this delta has raised many questions regarding processes that occur there that remain open today. Comparing long-term hydrometric observational data of Russian Federal Service for Hydrometeorology and Environmental Monitoring (Roshydromet) from the Khabarova polar station, located at the head of the delta not far from where the Lena River divides into its main branches, with field observations, which have been carried out since 2002 revealed new insights into the hydrological, hydrochemical, and geochemical processes within the delta. Three periods with various water volumes and intensity of fluvial processes were chosen from the long-term record of water and sediment discharge. The role of ice event (ice blockage and ice floating) during high water in reconfiguring branch channels and influencing the volume of sediment runoff was identified. Results were obtained quantifying the increase of water and sediment discharges in the middle part

U2 - 10.5194/bgd-10-20179-2013

DO - 10.5194/bgd-10-20179-2013

M3 - Article

VL - 10

SP - 20179

EP - 20237

JO - Biogeosciences Discussions

JF - Biogeosciences Discussions

SN - 1810-6277

ER -

ID: 5685256