Journal cover Journal topic
Biogeosciences An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

IF value: 3.480
IF 5-year value: 4.194
IF 5-year
CiteScore value: 6.7
SNIP value: 1.143
IPP value: 3.65
SJR value: 1.761
Scimago H <br class='widget-line-break'>index value: 118
Scimago H
h5-index value: 60
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

  03 Sep 2019

03 Sep 2019

Review status
This preprint is currently under review for the journal BG.

A numerical model study of the main factors contributing to hypoxia and its sub-seasonal to interannual variability off the Changjiang Estuary

Haiyan Zhang1,2, Katja Fennel1, Arnaud Laurent1, and Changwei Bian3 Haiyan Zhang et al.
  • 1Department of Oceanography, Dalhousie University, Halifax, Nova Scotia, Canada
  • 2School of Marine Science and Technology, Tianjin University, Tianjin, China
  • 3Physical Oceanography Laboratory/CIMST, Ocean University of China, and Qingdao National Laboratory for Marine Science and Technology, Qingdao, China

Abstract. A three-dimensional physical-biological model of marginal seas of China was used to analyze variations in hypoxic conditions and identify the main processes controlling their generation off the Changjiang Estuary. The model was validated against available observations and reproduces the observed temporal and spatial variability of hypoxia. Dissolved oxygen concentrations undergo a seasonal cycle, with minima generally occurring in August or September, and vary latitudinally with a longer duration of low-oxygen concentrations in the southern part of the hypoxic region. Interannual variations of hypoxic extent are primarily associated with variations in river discharge and wind forcing, with high river discharge promoting hypoxia generation. At synoptic time scales, strong wind events (e.g. typhoons) can disrupt hypoxic conditions. During the oxygen-depleted period (March–August), air–sea exchange acts as an oxygen sink in oversaturated surface waters. In the subsurface, biological oxygen consumption tends to dominate, but lateral physical transport of oxygen can be comparable during hypoxic conditions. Oxygen consumption in the water column exceeds that of the sediment when integrated over the whole water column, but sediment consumption is dominant below the pycnocline. Vertical diffusion of oxygen acts as the primary oxygen source below the pycnocline and shows a seasonal cycle similar to that of primary production. Advection of oxygen in the bottom waters acts as an oxygen sink in spring but becomes a source during hypoxic conditions in summer especially in the southern part of the hypoxic region, which is influenced by open-ocean intrusions.

Haiyan Zhang et al.

Interactive discussion

Status: final response (author comments only)
Status: final response (author comments only)
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

Haiyan Zhang et al.

Haiyan Zhang et al.


Total article views: 484 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
345 126 13 484 42 10 13
  • HTML: 345
  • PDF: 126
  • XML: 13
  • Total: 484
  • Supplement: 42
  • BibTeX: 10
  • EndNote: 13
Views and downloads (calculated since 03 Sep 2019)
Cumulative views and downloads (calculated since 03 Sep 2019)

Viewed (geographical distribution)

Total article views: 369 (including HTML, PDF, and XML) Thereof 368 with geography defined and 1 with unknown origin.
Country # Views %
  • 1



No saved metrics found.


No discussed metrics found.
Latest update: 18 Sep 2020
Publications Copernicus
Short summary
In coastal seas, low oxygen, which is detrimental to coastal ecosystems, is increasingly caused by man-made nutrients from land. This is especially so near mouths of major rivers including the Changjiang River in the East China Sea. Here a simulation model is used to identify the main factors determining low oxygen conditions in the region. High river discharge is identified as prime cause while wind and intrusions of open-ocean water modulate the severity and extent of low-oxygen conditions.
In coastal seas, low oxygen, which is detrimental to coastal ecosystems, is increasingly caused...