Seasonal and annual fluxes of nutrients and organic matter from large rivers to the Arctic Ocean and surrounding seas
Seasonal and annual fluxes of nutrients and organic matter from large rivers to the Arctic Ocean and surrounding seas
Date
2011-03
Authors
Holmes, Robert M.
McClelland, James W.
Peterson, Bruce J.
Tank, Suzanne E.
Bulygina, Ekaterina
Eglinton, Timothy I.
Gordeev, Viacheslav V.
Gurtovaya, Tatiana Y.
Raymond, Peter A.
Repeta, Daniel J.
Staples, Robin
Striegl, Robert G.
Zhulidov, Alexander V.
Zimov, Sergey A.
McClelland, James W.
Peterson, Bruce J.
Tank, Suzanne E.
Bulygina, Ekaterina
Eglinton, Timothy I.
Gordeev, Viacheslav V.
Gurtovaya, Tatiana Y.
Raymond, Peter A.
Repeta, Daniel J.
Staples, Robin
Striegl, Robert G.
Zhulidov, Alexander V.
Zimov, Sergey A.
Linked Authors
Person
Person
Person
Person
Person
Alternative Title
Citable URI
As Published
Date Created
Location
DOI
Related Materials
Replaces
Replaced By
Keywords
Abstract
River inputs of nutrients and organic matter impact the biogeochemistry of arctic
estuaries and the Arctic Ocean as a whole, yet there is considerable uncertainty about the
magnitude of fluvial fluxes at the pan-arctic scale. Samples from the six largest arctic
rivers, with a combined watershed area of 11.3 x 106 km2, have revealed strong seasonal
variations in constituent concentrations and fluxes within rivers as well as large
differences among the rivers. Specifically, we investigate fluxes of dissolved organic
carbon, dissolved organic nitrogen, total dissolved phosphorus, dissolved inorganic
nitrogen, nitrate, and silica. This is the first time that seasonal and annual constituent
fluxes have been determined using consistent sampling and analytical methods at the pan
arctic scale, and consequently provide the best available estimates for constituent flux
from land to the Arctic Ocean and surrounding seas. Given the large inputs of river water
to the relatively small Arctic Ocean, and the dramatic impacts that climate change is
having in the Arctic, it is particularly urgent that we establish the contemporary river
fluxes so that we will be able to detect future changes and evaluate the impact of the
changes on the biogeochemistry of the receiving coastal and ocean systems.
Description
Author Posting. © The Author(s), 2011. This is the author's version of the work. It is posted here by permission of Springer for personal use, not for redistribution. The definitive version was published in Estuaries and Coasts 35 (2012): 369-382, doi:10.1007/s12237-011-9386-6.