Anderson M C, Bland W L, Norman J M, Diak G D
Department of Soil Science, University of Wisconsin-Madison, Madison, WI 53706.
Cooperative Institute for Meteorological Satellite Studies, University of Wisconsin-Madison, WI 53706.
Plant Dis. 2001 Sep;85(9):1018-1026. doi: 10.1094/PDIS.2001.85.9.1018.
A method for predicting canopy wetness and humidity from remotely-acquired meteorological and radiation data is described. This method employs a surface energy balance model to scale from the above-canopy macroclimate to in-canopy microclimate conditions. Above-canopy temperature, vapor pressure, and wind speed inputs were obtained from objective analyses of hourly measurements from the synoptic weather network, while downwelling long- and shortwave radiation forcings were estimated from standard satellite observations. Precipitation (irrigation + rainfall) was the only input acquired in-field. Model predictions compared well with measurements of nighttime dew accumulation and relative humidity made in irrigated potato crops grown in central Wisconsin. Maximum dew amount measured in full canopies over four nights was reproduced to within 0.05 to 0.1 mm. The practical utility of this method to disease management was assessed by processing modeled and measured canopy microclimate data from two weather stations over three growing seasons through the BLITECAST disease forecasting system. Given the uncertainties inherent in the measurement of humidity, the model reasonably reproduced disease severity values generated from in-situ measurements in all but one case, where the canopy had suffered partial defoliation. Because the model simulates the microclimate within a healthy, uniform canopy, it may in many cases produce more reliable regional forecasts for plant disease than would a single set of in-situ measurements.
描述了一种根据遥感获取的气象和辐射数据预测冠层湿度的方法。该方法采用表面能量平衡模型,从冠层上方的宏观气候尺度转换到冠层内的微气候条件。冠层上方的温度、水汽压和风速输入数据来自对天气观测网络每小时测量数据的客观分析,而下沉长波和短波辐射强迫则根据标准卫星观测估算得出。降水量(灌溉量 + 降雨量)是唯一在田间获取的输入数据。模型预测结果与在威斯康星州中部种植的灌溉马铃薯作物中夜间露水积累和相对湿度的测量值进行了很好的对比。在四个夜晚全冠层测量的最大露水量再现误差在0.05至0.1毫米以内。通过BLITECAST病害预测系统,对三个生长季节中来自两个气象站的模型化和实测冠层微气候数据进行处理,评估了该方法在病害管理中的实际效用。考虑到湿度测量中固有的不确定性,除了一个冠层遭受部分落叶的情况外,该模型合理地再现了现场测量产生的病害严重程度值。由于该模型模拟的是健康、均匀冠层内的微气候,在许多情况下,它可能比单一的现场测量产生更可靠的植物病害区域预测。