摘要
In this paper a method is described of retrieving precipitable water from sun-photometer measurements.The quantitative relationship between water vapor transmission and precipitable water is established by means of LOWTRAN 7 model.Calibration of the water vapor absorption channel is made through a modified Langley method.The good agreement between the sun- photometer and radiosonde water vapor retrieval indicates that this method is feasible. The sun-photometer is operated at Hefei to monitor the precipitable water within one year period.Characteristics of both diurnal evolution and within-one-year variation of the precipitable water and their relation with synoptic system as well as surface dew-point temperature are presented and analyzed.Errors in the retrieved precipitable water from the sun-photometer measurements are also calculated and discussed.
In this paper a method is described of retrieving precipitable water from sun-photometer measurements.The quantitative relationship between water vapor transmission and precipitable water is established by means of LOWTRAN 7 model.Calibration of the water vapor absorption channel is made through a modified Langley method.The good agreement between the sun- photometer and radiosonde water vapor retrieval indicates that this method is feasible. The sun-photometer is operated at Hefei to monitor the precipitable water within one year period.Characteristics of both diurnal evolution and within-one-year variation of the precipitable water and their relation with synoptic system as well as surface dew-point temperature are presented and analyzed.Errors in the retrieved precipitable water from the sun-photometer measurements are also calculated and discussed.
