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Lena Delta hydrology and geochemistry: Long-term hydrological data and recent field observations. / Fedorova, I.; Chetverova, A.; Bolshiyanov, D.; Makarov, A.; Boike, J.; Heim, B.; Morgenstern, A.; Overduin, P.P.; Wegner, C.; Kashina, V.; Eulenburg, A.; Dobrotina, E.; Sidorina, I.

In: Biogeosciences, Vol. 12, No. 2, 2015, p. 345-363.

Research output: Contribution to journal › Article

Harvard

Fedorova, I, Chetverova, A, Bolshiyanov, D, Makarov, A, Boike, J, Heim, B, Morgenstern, A, Overduin, PP, Wegner, C, Kashina, V, Eulenburg, A, Dobrotina, E & Sidorina, I 2015, 'Lena Delta hydrology and geochemistry: Long-term hydrological data and recent field observations', Biogeosciences, vol. 12, no. 2, pp. 345-363. https://doi.org/10.5194/bg-12-345-2015

APA

Fedorova, I., Chetverova, A., Bolshiyanov, D., Makarov, A., Boike, J., Heim, B., Morgenstern, A., Overduin, P. P., Wegner, C., Kashina, V., Eulenburg, A., Dobrotina, E., & Sidorina, I. (2015). Lena Delta hydrology and geochemistry: Long-term hydrological data and recent field observations. Biogeosciences, 12(2), 345-363. https://doi.org/10.5194/bg-12-345-2015

Vancouver

Fedorova I, Chetverova A, Bolshiyanov D, Makarov A, Boike J, Heim B et al. Lena Delta hydrology and geochemistry: Long-term hydrological data and recent field observations. Biogeosciences. 2015;12(2):345-363. https://doi.org/10.5194/bg-12-345-2015

Author

Fedorova, I. ; Chetverova, A. ; Bolshiyanov, D. ; Makarov, A. ; Boike, J. ; Heim, B. ; Morgenstern, A. ; Overduin, P.P. ; Wegner, C. ; Kashina, V. ; Eulenburg, A. ; Dobrotina, E. ; Sidorina, I. / Lena Delta hydrology and geochemistry: Long-term hydrological data and recent field observations. In: Biogeosciences. 2015 ; Vol. 12, No. 2. pp. 345-363.

BibTeX

@article{033e6bb441ad4eae951bb68369be5579,
title = "Lena Delta hydrology and geochemistry: Long-term hydrological data and recent field observations",
abstract = "{\textcopyright} Author(s) 2015. The Lena River forms one of the largest deltas in the Arctic. We compare two sets of data to reveal new insights into the hydrological, hydrochemical, and geochemical processes within the delta: (i) long-term hydrometric observations at the Khabarova station at the head of the delta from 1951 to 2005; (ii) field hydrological and geochemical observations carried out within the delta since 2002. Periods with differing relative discharge and intensity of fluvial processes were identified from the long-term record of water and sediment discharge. Ice events during spring melt (high water) reconfigured branch channels and probably influenced sediment transport within the delta. Based on summer field measurements during 2005-2012 of discharge and sediment fluxes along main delta channels, both are increased between the apex and the front of the delta. This increase is to a great extent connected with an additional influx of water from tributaries, as well as an increase of suspended and dissolved",
author = "I. Fedorova and A. Chetverova and D. Bolshiyanov and A. Makarov and J. Boike and B. Heim and A. Morgenstern and P.P. Overduin and C. Wegner and V. Kashina and A. Eulenburg and E. Dobrotina and I. Sidorina",
year = "2015",
doi = "10.5194/bg-12-345-2015",
language = "English",
volume = "12",
pages = "345--363",
journal = "Biogeosciences",
issn = "1726-4170",
publisher = "European Geosciences Union",
number = "2",

}

RIS

TY - JOUR

T1 - Lena Delta hydrology and geochemistry: Long-term hydrological data and recent field observations

AU - Fedorova, I.

AU - Chetverova, A.

AU - Bolshiyanov, D.

AU - Makarov, A.

AU - Boike, J.

AU - Heim, B.

AU - Morgenstern, A.

AU - Overduin, P.P.

AU - Wegner, C.

AU - Kashina, V.

AU - Eulenburg, A.

AU - Dobrotina, E.

AU - Sidorina, I.

PY - 2015

Y1 - 2015

N2 - © Author(s) 2015. The Lena River forms one of the largest deltas in the Arctic. We compare two sets of data to reveal new insights into the hydrological, hydrochemical, and geochemical processes within the delta: (i) long-term hydrometric observations at the Khabarova station at the head of the delta from 1951 to 2005; (ii) field hydrological and geochemical observations carried out within the delta since 2002. Periods with differing relative discharge and intensity of fluvial processes were identified from the long-term record of water and sediment discharge. Ice events during spring melt (high water) reconfigured branch channels and probably influenced sediment transport within the delta. Based on summer field measurements during 2005-2012 of discharge and sediment fluxes along main delta channels, both are increased between the apex and the front of the delta. This increase is to a great extent connected with an additional influx of water from tributaries, as well as an increase of suspended and dissolved

AB - © Author(s) 2015. The Lena River forms one of the largest deltas in the Arctic. We compare two sets of data to reveal new insights into the hydrological, hydrochemical, and geochemical processes within the delta: (i) long-term hydrometric observations at the Khabarova station at the head of the delta from 1951 to 2005; (ii) field hydrological and geochemical observations carried out within the delta since 2002. Periods with differing relative discharge and intensity of fluvial processes were identified from the long-term record of water and sediment discharge. Ice events during spring melt (high water) reconfigured branch channels and probably influenced sediment transport within the delta. Based on summer field measurements during 2005-2012 of discharge and sediment fluxes along main delta channels, both are increased between the apex and the front of the delta. This increase is to a great extent connected with an additional influx of water from tributaries, as well as an increase of suspended and dissolved

U2 - 10.5194/bg-12-345-2015

DO - 10.5194/bg-12-345-2015

M3 - Article

VL - 12

SP - 345

EP - 363

JO - Biogeosciences

JF - Biogeosciences

SN - 1726-4170

IS - 2

ER -

ID: 3928027