Core Ideas Wind erosion results in loss of soil and associated C. Loss of C was measured from eroding fallow fields in eastern Washington. Eroded sediment was enriched in C compared with the parent soil. Carbon loss ranged from 0.4 to 18.5 kg C ha‐1 across 13 erosion events. Wind erosion of cropland negatively affects soil quality and productivity in the winter wheat (Triticum aestivum L.)–summer fallow (WW‐SF) region of the inland Pacific Northwest United States. Loss of soil diminishes the finite resource base and concurrent loss of soil organic C affects the inherent physical, chemical, and biological properties of the soil. This study aimed to quantify soil organic C loss from windblown summer fallow soils. Creep and Big Spring Number Eight samplers were used to trap sediment above an eroding soil during major wind events over an 8‐yr period. The C content of trapped sediment ranged from 6 to 11.6 g C per kg sediment. Enrichment ratios for C ranged from 0.6 to 1.9, indicating that the trapped sediment was generally enriched in C compared with the parent soil. Averaged across all sites and wind events, soil C loss from fields ranged from 0.4 to 18.5 kg C ha–1. The ongoing decline in soil organic C since the advent of dryland farming in the region 140 yr ago is most commonly attributed to degradation by microbes and oxidation. However, our data, combined with historic accounts of wind erosion in the WW‐SF region, strongly suggest that loss of soil organic C may also be caused by wind erosion. Conservation tillage has proven an effective strategy for reducing wind erosion in the WW‐SF region and thus farmers are encouraged to further adopt conservation tillage practices to retain soil C and thereby reduce the degradation of agricultural soils by wind erosion.