This study analyzes the influence of ENSO on tropical cloud clusters (TCCs) and TC formation in the WNP. TCCs are the precursors of TCs, which have an outside convective structure, contain mesoscale convection systems (MCSs) and last for more than 24 hours. In the WNP, a total of 2,248 TCCs are identified using infrared images, during July-October in 1981-2009. The analysis of this information shows that the numbers and activities of TCCs increase (decrease) in the eastern (western) part of the WNP during El Niño years, whereas the opposite situation occurs during La Niña years. However, the TC genesis productivities do not correlate significantly with ENSO index in the sub-regions of the WNP. The reason why the number of TCs changes in conjunction with the influence of ENSO in the sub-regions of WNP is because the activity of TCCs is affected by the environmental parameters which are controlled by the ENSO signal rather than by the variations in the TC genesis productivity. The environmental conditions of the developing and non-developing TCCs are also analyzed in this study to address the favorable conditions for the development of TCC.