Numerical study on the summertime patches of red tide in the adjacent sea of the Changjiang (Yangtze) River Estuary, China.

Abstract:

:High incident rates of red tide have occurred off the coast of the Changjiang (Yangtze) River Estuary in summer, resulting from a magnified population growth discharging substantial nutrient loads into this vicinity. The presence of elevated Chlorophyll-a concentrations (≥36.3 μg/l), low suspended sediment concentrations in surface and mid-layers (<10 mg/l), a strong saline front and surface water temperature gradient, veering surface winds, and a bimodal shape to the Changjiang Diluted Water (CDW) revealed two red tide patches appearing between August 6-13, 2010. Two distinguishable hydrodynamic driving mechanisms, connected to these incidents, are diagnosed. Field observations and numerical simulations determined a red tide patch in the northeastern offshore area is caused by a northeast transport of the CDW truncated by a northwest intrusion of the Taiwan Warm Current (TWC) as winds deviated. Red tide occurrence in the southern nearshore area originated from a plume front where CDW interfaces with the TWC.

journal_name

Mar Pollut Bull

authors

Qu D,Yu H,Sun Y,Zhao Y,Wei Q,Yu H,Kelly RM,Yuan Y

doi

10.1016/j.marpolbul.2019.04.027

subject

Has Abstract

pub_date

2019-06-01 00:00:00

pages

242-255

eissn

0025-326X

issn

1879-3363

pii

S0025-326X(19)30288-7

journal_volume

143

pub_type

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