( ( Latent heating ) ( ( is ( computed ( in ( ( ( two ways ) , ) ( corresponding ( ( ( ( to ( ( non-cumulus ( ( condensation and ) evaporation ) ) ( on ( the ( one hand ) ) ) ) ) , ) and ) ( to ( ( penetrating convection ) ( on ( the other ) ) ) ) ) ) ) ) ) ) . ) )
(ROOT (S (NP (JJ Latent) (NN heating)) (VP (VBZ is) (VP (VBN computed) (PP (IN in) (NP (NP (CD two) (NNS ways)) (, ,) (NP (NP (JJ corresponding)) (PP (PP (TO to) (NP (NP (JJ non-cumulus) (NN condensation) (CC and) (NN evaporation)) (PP (IN on) (NP (DT the) (CD one) (NN hand))))) (, ,) (CC and) (PP (TO to) (S (VP (VBG penetrating) (NP (NN convection)) (PP (IN on) (NP (DT the) (JJ other)))))))))))) (. .)))
Latent heating is computed in two ways, corresponding to non-cumulus condensation and evaporation on the one hand, and to penetrating convection on the other.
(ROOT (S (NP (NN Evaporation) (CC and) (NN condensation)) (VP (VBP are) (ADJP (JJ similar) (SBAR (IN because) (S (NP (DT both)) (VP (VBP are) (VP (VBN caused) (PP (IN by) (NP (NP (NNS changes)) (PP (IN in) (NP (NN heat) (NN energy))))))))))) (. .)))