Abstract
Large rivers are key components of the land-ocean branch of the global water and biogeochemical cycles. River discharges can have important influences on physical, biological, optical, and chemical processes in coastal oceans. It is, therefore, of importance to routinely monitor the time-varying dispersal patterns of river plumes. The European Space Agency (ESA) Soil Moisture and Ocean Salinity (SMOS) and the NASA Soil Moisture Active Passive (SMAP) satellites provide Sea Surface Salinity (SSS) observations capable of characterizing the spatial and temporal variability of major river plumes. The main objective of this study is to examine the consistency of SSS products, from these two missions, and two in-situ gridded salinity products in depicting SSS variations on seasonal to interannual time scales within a few hundred kilometers of major river mouths. We show that SSS from SMOS and SMAP satellites have good consistency in depicting seasonal and interannual SSS variations near major river mouths. The two gridded in-situ products underestimate these variations substantially. This underestimation, most notably associated with the low SSS season following the high-discharge season, is attributable to the limited in-situ sampling of the river plumes when they are the most active. This work underscores the importance of using satellite SSS to study river plumes, as well as to evaluate and constrain models.
Highlights
We show that Sea Surface Salinity (SSS) from Soil Moisture and Ocean Salinity (SMOS) and Soil Moisture Active Passive (SMAP) satellites have good consistency in depicting seasonal and interannual SSS variations near major river mouths
Seasonal SSS maps are computed by averaging maps over the common period May 2015 to November 2020 each month of different years
Seasonal SSS maps are computed by averaging maps over the common period May 2015 to 2020 each month of different
Summary
Large rivers are key components of the land-ocean branch of the global water and biogeochemical cycles. River runoff represents only 10% of the total freshwater input to the ocean [1], it can have important influences on physical, biological, optical, and chemical processes in the coastal oceans. Large riverine freshwater inputs into the ocean affects ocean currents and air–sea interactions through their effects on near-surface stratification, including the formation of barrier layer that isolates colder subsurface waters from warmer surface waters. The effect on stratification and mixing has implications for ecosystems and biogeochemistry, for instance, by regulating the nutrient supply from the subsurface to surface waters and affecting the biological activity in the surface layer [2,3,4]
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