{"thcode":62,"term":{"code":"WC-661","name":"Reverse Estuarine Flow","parent":"WC-640","scope":"Hydroform Type: An estuarine circulation where evaporation greatly exceeds freshwater input, as in hot dry climes, salinity is concentrated within the estuarine basin. This results in a salinity maximum in the estuary that can far exceed seawater salinity."},"uf":[],"bt":[{"code":"WC-640","name":"Residual Current","parent":"WC-627","scope":"Hydroform: Current movement resulting from asymmetry in tidal flow?notably within a partially enclosed estuary or embayment?that results in characteristic estuarine circulation patterns."},{"code":"WC-627","name":"Current","parent":"WC-C012","scope":"Hydroform Class: Water that is undergoing coherent mass movement, either as laminar or turbulent flow, relative to surrounding waters and fixed structural, landform or geologic features. ..."},{"code":"WC-C012","name":"Hydroform","parent":"WC-C001","scope":null},{"code":"WC-C001","name":"Water Column","parent":"root","scope":null},{"code":"root","name":"CMECS","parent":null,"scope":"Coastal and Marine Ecological Classification Standard: Category terms encompassing waters from the head of tide or inland incursion of ocean salinity to the splash zone of the coasts to the deepest portions of the oceans and the deep waters of the Great Lakes."}],"nt":[],"rt":[]}