Urbanization　has　disrupted　the　energy　balance　of　natural　surfaces,　leading　to　the　formation　and　intensification　of　urban　heat　island　(UHI)　phenomenon.　Current　research　on　the　relationship　between　surface　energy　balance　(SEB)　and　UHI　mainly　focuses　on　either　a　macro　perspective　of　large-scale　regions　or　a　micro　perspective　based　on　numerical　microclimate　simulations.　However,　there　are　still　relatively　few　studies　conducted　on　the　local　scale　of　cities.　Here,　we　investigated　the　relationships　between　seasonal　SEB　and　land　surface　temperature　(LST)　based　on　local　climate　zones　(LCZ)　and　explored　the　impact　of　three-dimensional　(3D)　urban　morphology　on　SEB.　Our　results　revealed　that:　(1)　urban　building　spaces　have　relatively　higher　LST,　sensible　heat　flux,　and　storage　heat　flux,　but　lower　net　radiation　and　latent　heat　flux,　compared　to　urban　blue　and　green　spaces;　(2)　among　LCZ　built　types,　the　compact　and　large　low-rise　buildings　have　high　LST　and　heat-inducing　energy　fluxes,　while　the　compact　and　open　high-rise　buildings　exhibit　the　opposite　situation;　(3)　the　component　proportions　of　SEB　fluxes　exhibit　a　more　significant　linear　correlation　with　UHI　intensity　compared　to　the　relative　differences　between　SEB　fluxes;　and　(4)　3D　building　morphology　has　a　higher　relative　importance　in　influencing　the　variations　of　surface　energy　balance　ratio　(SEBR)　components　than　3D　vegetation　morphology.　Specifically,　building　height　has　the　greatest　impact　on　the　seasonal　variations　of　SEBR　components,　while　the　3D　urban　greening　ratio　has　relatively　high　importance　among　vegetation　morphology.　These　findings　enable　us　to　better　consider　local　UHI　effect　from　the　perspective　of　SEB.