RT Journal Article
T1 Time periodic solutions for a diffusive energy balance model in climatology
A1 Díaz Díaz, Jesús Ildefonso
A1 Badii, M
AB We prove the existence of a periodic solution to the problem u(t) - Delta(p)u + R-e(x,u) is an element of mu Q(x,t)beta(u) in M x R, assumed p greater than or equal to 2, M a compact connected and oriented bidimensional Riemannian manifold without boundary, beta(u) a bounded maximal monotone graph (the coalbedo), Q(x, t) a time periodic function (the incoming solar radiation flux) and R-e a time independent strictly increasing function of the surface temperature u (the Earth emitted energy)
PB Academic Press
SN 0022-247X
YR 1999
FD 1999-05-15
LK https://hdl.handle.net/20.500.14352/57369
UL https://hdl.handle.net/20.500.14352/57369
LA eng
NO DGICYT (Spain
NO G.N.A.F.A.-C.N.R. M.U.R.S.T
DS Docta Complutense
RD 6 abr 2025