Taihang mountain > Hebei east plain > Yanshan hills > Hebei north plateau. The evaporation rate was gradually increasing from north to south. The drop rate of pan evaporation was: spring > autumn > winter > summer. Evaporation capacity and influence factors are analyzed. The results show that temperature daily range, sunshine duration and average wind speed are the major causes of the evaporation reduction in the BeijingTianjinHebei region. In the plain area, average wind speed is the dominant factor. In the mountainous and plateau areas, sunshine duration is the dominant factor."/>