{"thcode":62,"term":{"code":"WC-659","name":"Fjord Circulation","parent":"WC-640","scope":"Hydroform Type: Circulation in estuaries that possess a sill at the seaward end, inhibiting inflow of seawater into the bottom waters. ..."},"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":[]}