The role of wind on the detachment of low salinity water in the Changjiang Estuary in summer

Abstract

[1] Two detachment processes of low salinity water (LSW) in the Changjiang Estuary in July 2006, and the role of wind on detaching the LSW in particular, are explored with a three-dimensional numerical model. The real-case simulation and the sensitivity experiments results show that wind plays a crucial role in the detachment events and is highlighted in three aspects. First, wind is the most important dynamic factor in the two detachment processes of the LSW. Wind mixing, wind-driven northward current and wind-induced upwelling are three driving forces on detaching the LSW, which increase the salinity in the upper layer in the detachment region along the 30 m isobath and separate the offshore LSW from the nearshore main body of LSW. The diagnostic analysis further indicates that the increase of salinity in the detachment region is mainly due to northward current which transports high salinity water from the south. Second, a critical wind speed, namely a southeasterly wind above 8.0 m/s, is found to be related to the timing of the detachment events. A sensitivity experiment further confirms this critical wind speed and no detachment occurs when the wind speed is below 8.0 m/s. Third, the southwesterly wind plays a key role in the magnitude of the spatial size of the detached LSW. Before the detachment occurs, a persistent southwesterly wind induces northeastward expansion of the LSW and consequently forms larger LSW offshore after detachment, which is verified by another sensitivity experiment with modified wind direction.

Real‐time monitoring of nutrients in the Changjiang Estuary reveals short‐term nutrient‐algal bloom dynamics

“…During the first period of salinity decline observed in the buoy study, from 9–12 September, the daily averaged salinity decrease appeared to be mainly controlled by neap tidal mixing with quite weak wind (as estimated by tidal water level) and was accompanied by and increases coming from CDW (Figure ). During the second period of salinity decline, from 17–23 September, which occurred under the spring tide, a southeasterly wind of 2.7–9.4 m/s prevailed for about 6 days (Figures a and e), which favored CDW expansion or LSW detachment [ Xuan et al ., ]. After a short period of weakening winds, by 23 September, the northeasterly winds strengthened suddenly and a second SDA started.…”

Role of pulsed winds on detachment of low salinity water from the Pearl River Plume: Upwelling and mixing processes

“…Xuan et al . [] concluded that the detachment only occurred under the southeasterly wind with speed higher than 8.0 m s − 1 , related to wind‐induced mixing, northward alongshore currents, and upwelling.…”

Distribution of hypoxia and pycnocline off the Changjiang Estuary, China

“…The summer extension of the Changjiang diluted water (CDW) has received widespread attention (e.g., Mao et al, 1963;Wu et al, 2011;Xuan et al, 2012). The discharge of the Changjiang River can reach more than 50,000 m 3 /s during the summer.…”