海洋では貯熱量 S が非常に大きく、C海域ではほぼ-200~+200W/m2
の間で季節変化している。海洋熱発散量FDIV は北方の A 海域
では、プラス・マイナスで年間の平均値はゼロに近いのだが、黒潮の影響の
ある南方の C 海域では、概略-200~0 W/m2の間にあり、年平均値
はゼロにならない。
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