Abstract
The integral property of hydrometeorological fields (atmospheric pressure, wind speed, wind waves, temperature and salinity of seawater, sea currents) is their spatial—time variability caused by superposition and interaction of a large number of factors. Characteristic ranges of variability are interannual variability (cyclicity of fluctuations more than one year), annual cycles, synoptic variability (time scale of fluctuations from one day to several days), daily cycles, small-scale fluctuations (cyclicity from several seconds to one hour). The presence of multiscale variability causes nonstationarity of hydrometeorological processes. Variety of active factors results in spatial heterogeneity of fields (stratification of surface layer and seawater, movement of baric formations in an atmosphere and mesoscale eddies in oceans and seas).
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Boukhanovsky, A., Rozhkov, V., Degtyarev, A. (2001). Peculiarities of Computer Simulation and Statistical Representation of Time—Spatial Metocean Fields. In: Alexandrov, V.N., Dongarra, J.J., Juliano, B.A., Renner, R.S., Tan, C.J.K. (eds) Computational Science — ICCS 2001. ICCS 2001. Lecture Notes in Computer Science, vol 2073. Springer, Berlin, Heidelberg. https://doi.org/10.1007/3-540-45545-0_55
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