lena delta hydrology and geochemistry: long-term hydrological data and recent field observations
Clicks: 207
ID: 247425
2015
Article Quality & Performance Metrics
Overall Quality
Not rated
Combines reader engagement with the AI quality analysis. This
article has not been analysed, so there is no overall score —
reader engagement is measured and shown alongside.
Reader Engagement
Steady Performance
30.0
/100
207 views
48 readers
AI Quality Assessment
Not analyzed
Readership in this journal
SteadyRanked #65 of 345 articles by views in tetrahedron letters
Most read
Least read
Bar heights use a square-root scale. Only the 120 most-read articles are drawn; the journal has 345 in total.
Mint this article as an NFT
Not yet mintedCreate a permanent, verifiable on-chain record of this article on the Scimatic Network. The NFT is held in your Journament account, and you can withdraw it to your own wallet at any time.
5
SUSD
one-off · no wallet required
Abstract
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 material released from the ice
complex. Summer concentrations of major ion and biogenic substances along the
delta branches are partly explained by water sources within the delta, such
as thawing ice complex waters, small Lena River branches and estuarine areas.
| Reference Key |
fedorova2015biogeoscienceslena
Use this key to autocite in the manuscript while using
SciMatic Manuscript Manager or Thesis Manager
|
|---|---|
| Authors | ;I. Fedorova;A. Chetverova;D. Bolshiyanov;A. Makarov;J. Boike;B. Heim;A. Morgenstern;P. P. Overduin;C. Wegner;V. Kashina;A. Eulenburg;E. Dobrotina;I. Sidorina |
| Journal | tetrahedron letters |
| Year | 2015 |
| DOI |
10.5194/bg-12-345-2015
|
| URL | |
| Keywords |
Citations
No citations found. To add a citation, contact the admin at info@scimatic.org
Comments
No comments yet. Be the first to comment on this article.