In recent years, the drought phenomenon has caused a severe reduction in surface waters in the White village basin. This has increased the utilization of groundwater resources and intensified the simulate water level of underground water tablecloths in this basin. The aim of this study was to investigate the response of groundwater in the White village area towards the occurrence of drought and moist and the correlation between them. Since his diagnosis, meteorological drought and hydrological involuntary (SRI) pulled his accountant. Then, Pearson correlation and dronght to arrange the ba-n benefited by Paz stake astandard berh involuntary (SPI), the source of geohydrological dronght (SGI) and Dubai astandard stake cross-correlation between indices were calculated for data on time scale (1, 3, level changes with the process of changes in meteorological and hydrological 6, 12, 18, 24) months. The results showed that drought climate changes are severe and variable, but the drought status of groundwater has a more constant trend and its changes are not high. Also, the trend of groundwater waters that have increased from about 8 to 9 months after the date of the conditions were investigated in two areas of downstream and downstream of the basin to determine the severe changes and the low level of groundwater levels in the last two decades have human or natural origin. According to the results, it was determined that by the beginning of the drought trend of meteorology from January of the year. This is especially visible to the underground correlation with the changes in hydrological and geohydrological conditions in aforementioned drought process. According to the results, it can be stated that the intensification of meteorological, hydrological and geohydrological droughts in the study area was originated from 1387. The results of this study also indicate that the changes in meteorological conditions in long-term scales such as 12, 18 and 24 months have the highest correlation values showed that the changes in geohydrological conditions with the Aspas plain range. Second, in relation to geohydrological conditions, these correlations will be reached peak for 2 to 4 months delay for 12, 18 and 24 hydrological conditions of the region are associated with the weather conditions month, 8 to 11 months for the 9th to 18th month. This is while changes in without delay or with short-term delays. On the other hand, the geohydrologic. changes in hydrological conditions have more correlation than meteorological changes. This means that the feeding of groundwater in this plain is mostly carried out by surface flows and rivers in order to reserve the basin level and its formations. Of course, it should be considered that the changes of meteorological drought will not lead to hydrological changes and Keywords: Drought, SPI , SRI , SGI , Aspas Plain