Описание: Here climate signals are examined in terms of changes of layer depth, layer thickness, layer temperature/salinity, spicity and others. In addition to the traditional Theta-S diagram, the sigma-pi (potential density - potential spicity) diagram can also be used in analyzing water mass property distribution and climate variability.
ООО "Логосфера " Тел:+7(495) 980-12-10 www.logobook.ru