The results show time interval of atmospheric forcing gives rise to significant difference in net solar radiation and latent heat in siberia area 西伯利亞地區(qū)的單點(diǎn)試驗(yàn)表明不同時(shí)間間隔的邊界強(qiáng)迫對(duì)地表吸收的凈短波輻射和釋放的潛熱影響較大。
The simulations of ground temperature and earth absorbed net solar radiation are lower than the observation . sensible heat and latent heat are also lower than the observation 由于模式模擬的地溫偏低,凈的短波輻射偏小,則模擬的感熱和潛熱值偏小。