Wetness was measured in a soybean canopy at West Lafayette, IN, during the summer of 2005 using resistance-grid wetness sensors located at three heights representative of the top, mid-level, and lowest trifoliate of the canopy. For additional data, a temperature and relative humidity probe and anemometer were placed at approximately 8 cm above the canopy height. Measurements were taken at three-minute intervals for 47 days. Wetness sensors were checked for accuracy before and after the experiment, while in-field data logger checks confirmed accuracy of the other instruments.
Over the course of the field experiment, 24 events of interest were studied; seven dew events and seventeen late afternoon or evening rains. The dew events were then compared against the rain events to examine differences in the temporal formation and dry-down periods. Dew events themselves were compared and analyzed for duration length, differences in formation and dry-down periods, and other quantifiable factors. Two days of human observation after heavy dewfall events were also conducted and compared to dry-down readings by the wetness sensors. An average length of time for wetness events was established, and attempts were made at describing the dry-down process of early morning wetness transfer throughout the canopy.