A thermal parametric model has been developed for analyzing observed r
egional sea temperature profiles based on a layered structure of tempe
rature fields (mixed layer, thermocline, and deep layers). It contains
three major components: (1) a first-guess parametric model, (2) high-
resolution profiles interpolated from observed profiles, and (3) fitti
ng of high-resolution profiles to the parametric model. The output of
this parametric model is a set of major characteristics of each profil
e: sea surface temperature, mixed-layer depth, thermocline depth, ther
mocline temperature gradient, and deep layer stratification. Analyzing
nearly 15,000 Yellow Sea historical (1950-1988) temperature profiles
(conductivity-temperature-depth station, 4825; expendable bathythermog
raph, 3213; bathythermograph, 6965) from the Naval Oceanographic Offic
e's Master Oceanographic Observation Data Set by this parametric model
, the Yellow Sea thermal field reveals dual structure: one layer (vert
ically uniform) during winter and multilayer (mixed layer, thermocline
, sublayer) during summer. Strong seasonal variations were also found
in mixed-layer depth, thermocline depth, and thermocline strength.