During the Antarctic ice-melting season, high-resolution sea ice data
were collected with the video monitoring system aboard the icebreaker
Shirase along with the monitoring of temperature and salinity in the u
pper ocean. On the basis of these data, relationships among sea ice co
ncentration, temperature, and salinity are investigated. In the ice in
terior region away from the ice-free ocean, ice concentration is negat
ively correlated with temperature and positively correlated with salin
ity for the spatially averaged data, which suggests chat the local bal
ances of heat and salt nearly hold in a bulk area. At the ice margin,
ice concentration is negatively correlated with both temperature and s
alinity, suggesting that the local balances are overwhelmed by the eff
ects of ice advection. The expendable bathythermograph profiles at the
ice margin also show that considerable amount of sea ice was advected
into the ice-free ocean and subsequently melted there. It is pointed
out that a polynya works as an ''ice-melting factory'' in summer; it a
bsorbs solar radiation during the period of opening, and then melts th
e ice advected there. From a heat budget analysis and ocean structure
in the melting season, we propose a simple ice-upper ocean coupled mod
el in which sea ice melts on the bottom and lateral faces with the hea
t source supplied to the open water area by solar radiation. The relat
ions among ice concentration, temperature, and salinity derived from t
he model are consistent with the observed relations. The analytic solu
tion for the no lateral melting case shows that the concentration-temp
erature relation converges to a certain asymptotic curve with time, wh
ich explains that the temperature-concentration plot shows a similar r
elation for any region. Dependence of the relations among ice concentr
ation, temperature, and salinity on the spatial scale is also discusse
d.