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However, the monsoonal climate brings rain during December to April, and may result in river plume impingement and stratification.
To examine the effects of latitude, wind and river discharge on the river plume, we designed several numerical experiments.
Changes in river discharge influence stratification in the UGoT but have little effect on the behavior of the river plume.
Gan, J., Li, L., Wang, D. & Guo, X. Interaction of a river plume with coastal upwelling in the northeastern South China Sea.
Here, we apply a numerical model to the Upper Gulf of Thailand (UGoT) to examine a river plume in low latitudes.
Estimates of carbon ingestion rates and δ13C in copepods from the river plume areas indicated that terrestrial carbon could account for a significant percentage of the copepod body carbon (20 50%) during periods of food limitation.
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River plumes of the Herbert, Tully, Murray, Hull, Johnstone, and Mulgrave/Russell rivers were noticeably changed, with some paths diverted.
South-east Queensland had14 inches of rain in three hours, causing flash floods that formed distinct river plumes along the coastline.
Most previous studies focus on river plumes in middle and high latitudes with few studies examining those in low latitude regions.
In the Mid-Atlantic coastal ocean, salinity is critical for understanding circulation patterns, river plumes, and transport, which in turn impact the status of the ecosystem.
Here, with extensive in situ measurements of surface pCO2, the MeSAA, originally developed for the summertime East China Sea, was tested in the northern Gulf of Mexico (GOM) where river plumes dominate water's biogeochemical properties during summer.
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