TI: Variations in the underlying surface temperature and the problem of 
    closure of the heat balance equation
LA: Russian
AU: Kukharets_VP, Tsvang_LR
NA: RUSSIAN ACAD SCI,OBOUKHOV INST ATMOSPHER PHYS,PYZHEVSKII PER 3,MOSCOW
    109017,RUSSIA
JN: IZVESTIYA AKADEMII NAUK FIZIKA ATMOSFERY I OKEANA, 1999, Vol.35, 
    No.2, pp.207-214
IS: 0002-3515
DT: Article
AB: The results of measurements of the components of the heat balance 
    equation fur the land surface and of time variations in land surface 
    temperature are given. It is shown that the daily regime of the 
    exchange between the atmosphere and the underlying surface is 
    essentially nonstationary. In this connection, the authors propose 
    that, instead of the heat balance equation, the heat influx equation 
    should be used in studying heat balance. 
KP: TURBULENT EXCHANGE, ENERGY-BALANCE, FLUXES, INHOMOGENEITIES, 
    RADIATION, LAYER
CR: ANDRE_JC, 1990 Vol.50 p.77, BOUND-LAY METEOROL
    BOLLE_HJ, 1993 Vol.11 p.173, ANN GEOPHYS
    BRAUD_I, 1993 Vol.66 p.173, BOUND-LAY METEOROL