TY - JOUR
AU - Blender, Richard
AB - The 1 ∕ f spectrum of the ocean surface temperature in the Atlantic and Pacific midlatitudes is explained by a simple vertical diffusion model with a shallow mixed layer on top of a deep ocean. The model is forced at the air-sea interface with the total surface heat flux from a 1000 year climate simulation. The analysis reveals the role of ocean advection and substantiates estimates of internal thermal diffusivities.
TI - 1 ∕ f model for long-time memory of the ocean surface temperature
JF - Physical Review E
DO - 10.1103/PhysRevE.70.037301
DA - 2004-09-01
UR - https://www.deepdyve.com/lp/american-physical-society-aps/1-f-model-for-long-time-memory-of-the-ocean-surface-temperature-AC3dSz8MrO
VL - 70
IS - 3
DP - DeepDyve
ER -