AbstractBy analyzing the data collected over a rice paddy field in China, the occurrence of large drag coefficient in light winds (U ≤ 1ms−1) under near‐neutral conditions (−0.1 ≤ z/L ≤ 0.1) is analyzed in this study. It is found that, with the use of either vector‐ or scalar‐averaged wind speed, the drag coefficient under near‐neutral conditions (CDN) always increases with the decrease of wind speed. Such behavior of CDN cannot be interpreted by the change of aerodynamic roughness length z0 because it would need to be enlarged by an order of magnitude. While in light winds, the nonlocal transport, which is caused by large‐scale eddies and overlooked by traditional Monin‐Obukhov Similarity theory, is found to be the main cause of increased CDN. At last, a fixing term related to nonlocal effects is proposed based on our observation, and its applicability is verified with two AmeriFlux observation sites with a landscape of forest and savanna, respectively.