Abstract. Summer crop production on slow-draining Vertosols in a sub-tropical climate has the potential for large emissions of soil nitrous oxide (N 2 O) from denitrification of applied nitrogen (N) fertiliser. While it is well established that applying N fertiliser will increase N 2 O emissions above background levels, previous research in temperate climates has shown that increasing N fertiliser rates can increase N 2 O emissions linearly, exponentially or not at all. Little such data exists for summer cropping in sub-tropical regions. In four field experiments at two locations across two summers, we assessed the impact of increasing N fertiliser rate on both soil N 2 O emissions and crop yield of grain sorghum (Sorghum bicolor L.) or sunflower (Helianthus annuus L.) in Vertosols of sub-tropical Australia. Rates of N fertiliser, applied as urea at sowing, included a nil application, an optimum N rate and a double-optimum rate.Daily N 2 O fluxes ranged from -3.8 to 2734 g N 2 O-N ha -1 day -1 and cumulative N 2 O emissions ranged from 96 to 6659 g N 2 O-N ha -1 during crop growth. Emissions of N 2 O increased with increased N fertiliser rates at all experimental sites, but the rate of N loss was five times greater in wetter-than-average seasons than in drier conditions. For two of the four experiments, periods of intense rainfall resulted in N 2 O emission factors (EF, percent of applied N emitted) in the range of 1.2-3.2%. In contrast, the EFs for the two drier experiments were 0.41-0.56% with no effect of N fertiliser rate. Additional 15 N mini-plots aimed to determine whether N fertiliser rate affected total N lost from the soil-plant system between sowing and harvest. Total 15 N unaccounted was in the range of 28-45% of applied N and was presumed to be emitted as N 2 O + N 2 . At the drier site, the ratio of N 2 (estimated by difference) to N 2 O (measured) lost was a constant 43%, whereas the ratio declined from 29% to 12% with increased N fertiliser rate for the wetter experiment.Choosing an N fertiliser rate aimed at optimum crop production mitigates potentially high environmental (N 2 O) and agronomic (N 2 + N 2 O) gaseous N losses from over-application, particularly in seasons with high intensity rainfall occurring soon after fertiliser application.