CAUTIONARY REMARKS ON THE SPECTRAL INTERPRETATION OF TURBULENT FLOWS

[11] PHYTOPLANKTON PATCHINESS INDICATES THE FLUCTUATION SPECTRUM OF MESOSCALE OCEANIC STRUCTURE [J]. NATURE, 1980, 288 (5787) : 157 - 159

[12] HOLLADAY CG, 1975, J PHYS OCEANOGR, V5, P761, DOI 10.1175/1520-0485(1975)005<0761:MVOSST>2.0.CO

[13] 2

[14] THE LOCAL-STRUCTURE OF TURBULENCE IN INCOMPRESSIBLE VISCOUS-FLUID FOR VERY LARGE REYNOLDS-NUMBERS [J]. PROCEEDINGS OF THE ROYAL SOCIETY OF LONDON SERIES A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, 1991, 434 (1890): : 9 - 13

[15] INERTIAL RANGES IN 2-DIMENSIONAL TURBULENCE [J]. PHYSICS OF FLUIDS, 1967, 10 (07) : 1417 - +

[16] LESIEUR M, 1981, NATURE, V294, P673, DOI 10.1038/294673a0

[17] SPATIAL SPECTRA OF OCEAN SURFACE TEMPERATURE [J]. JOURNAL OF GEOPHYSICAL RESEARCH, 1970, 75 (33): : 6872 - &

[18] THE IMPORTANCE OF PHASE IN SIGNALS [J]. PROCEEDINGS OF THE IEEE, 1981, 69 (05) : 529 - 541

[19] SAFFMAN PG, 1971, STUD APPL MATH, V50, P377

[20] Salmon R., 1978, Geophysical and Astrophysical Fluid Dynamics, V10, P25, DOI 10.1080/03091927808242628

[11] PHYTOPLANKTON PATCHINESS INDICATES THE FLUCTUATION SPECTRUM OF MESOSCALE OCEANIC STRUCTURE [J]. NATURE, 1980, 288 (5787) : 157 - 159

[12] HOLLADAY CG, 1975, J PHYS OCEANOGR, V5, P761, DOI 10.1175/1520-0485(1975)005<0761:MVOSST>2.0.CO

[13] 2

[14] THE LOCAL-STRUCTURE OF TURBULENCE IN INCOMPRESSIBLE VISCOUS-FLUID FOR VERY LARGE REYNOLDS-NUMBERS [J]. PROCEEDINGS OF THE ROYAL SOCIETY OF LONDON SERIES A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, 1991, 434 (1890): : 9 - 13

[15] INERTIAL RANGES IN 2-DIMENSIONAL TURBULENCE [J]. PHYSICS OF FLUIDS, 1967, 10 (07) : 1417 - +

[16] LESIEUR M, 1981, NATURE, V294, P673, DOI 10.1038/294673a0

[17] SPATIAL SPECTRA OF OCEAN SURFACE TEMPERATURE [J]. JOURNAL OF GEOPHYSICAL RESEARCH, 1970, 75 (33): : 6872 - &

[18] THE IMPORTANCE OF PHASE IN SIGNALS [J]. PROCEEDINGS OF THE IEEE, 1981, 69 (05) : 529 - 541

[19] SAFFMAN PG, 1971, STUD APPL MATH, V50, P377

[20] Salmon R., 1978, Geophysical and Astrophysical Fluid Dynamics, V10, P25, DOI 10.1080/03091927808242628