ESA’s SMOS water mission has taken another step forward by demonstrating that it will lead to a better understanding of ocean circulation. Using preliminary data, scientists can clearly see how surface currents affect the ‘Amazon plume’ in the open sea.
The Soil Moisture and Ocean Salinity (SMOS) mission has been delivering observations of ‘brightness temperature’ to the science community since mid-July. As a measure of radiation emitted from Earth’s surface, this information can be used to derive global maps of soil moisture every three days and maps of ocean salinity at least every 30 days.
By consistently mapping soil moisture and ocean salinity, SMOS will advance our understanding of the exchange processes between Earth’s surface and atmosphere ““ the water cycle ““ and help improve weather and climate models. In addition, these data will be of practical use for agriculture and water resource management.
Soil moisture and ocean salinity data products will be released later this month, but scientists are very encouraged by what they are already seeing.
Talking about observations that relate to ocean salinity, Nicolas Reul from Ifremer said, “One of the dramatic steps forward achieved with SMOS is that we now have the ability to track the movement of low-salinity surface waters, particularly those resulting from large ‘plumes’ such as the Amazon.
“Observations between mid-July and mid-August clearly show how the North Brazilian Current transports fresh water from the Amazon River as the current flows across the mouth of the river. These observations confirm the excellence of the data we are already getting from SMOS.”
Discharge from the Amazon River, the Amazon plume, amounts to around 15% of the global input of fresh water into the ocean. The migration of the plume, however, varies seasonally. During the first half of the year the river water generally disperses over a broad area to the northwest, towards the Caribbean Sea, but in the second half of the year the plume flows around the North Brazil Current and is carried back eastwards.
The migration of the Amazon plume results in significant differences in the salinity of the surface ocean water, so it was expected that SMOS would reveal the intricacies of these variations.
“Over the last weeks we have been able to track how the Amazon freshwater plume curves back on itself at this time of year as large North Brazilian Current eddies form northwest of the river mouth,” said Dr Reul.
“At the same time, the Orinoco plume has also been clearly visible as a tongue of fresh water entering the Tropical Atlantic along the windward side of the Caribbean islands.
“These observations are a good example of how well SMOS is performing and they show us that the mission can provide data on temporal sea-surface variability at scales of less than a week.”
Along with temperature, variations in ocean salinity drive global three-dimensional ocean-circulation patterns. This conveyor-like circulation is an important component of Earth’s heat engine and crucial in regulating weather and climate. Ocean salinity data from SMOS are therefore expected to greatly improve our knowledge of the conditions that influence these circulation patterns and thus climate.
Image 1: The Soil Moisture and Ocean Salinity (SMOS) mission makes global observations of soil moisture over Earth’s landmasses and salinity over the oceans. Variations in soil moisture and ocean salinity are a consequence of the continuous exchange of water between the oceans, the atmosphere and the land ““ Earth’s water cycle. Credits: ESA – AOES Medialab
Image 2: The image, derived from SMOS data in July 2010, clearly shows the plume of fresh Amazon River water as it enters the Atlantic Ocean. Credits: I. Corbella, UPC / Google Earth
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