A composite analysis of diurnal cycle of GPS precipitable water vapor in central Japan during Calm Summer Days

• DOI: 10.1007/s00704-006-0293-x
• Publication Date: 2007-07-04T13:45:40Z
• Authors: G. Li; F. Kimura; T. Sato; D. Huang
• Keywords: Noon; Diurnal cycle; Diurnal temperature variation; Precipitable water; Annual cycle

The diurnal variations of water vapor in central Japan were investigated with GPS-derived precipitable water (PWV) and surface meteorological data as classified to three kinds of locations. Twenty-five clear days in central Japan in August 2000 were investigated to clarify the role of water vapor in the nocturnal maximum in the diurnal cycle of convective rainfall. The diurnal variations of PWV and some meteorological factors were composite during the selected days at 6 stations. The PWV shows a clear diurnal cycle with the amplitude of 3.4 mm to 8.8 mm and changes little during the period from the morning to noon. The daily amplitude of PWV is the largest in basin and smallest in plain although mean of PWV keeps high value in plain. A typical feature of the diurnal variation in central Japan is a maximum appearing in the evening. The time of maximum is from 1800 LST to 2000 LST, and minima appears at noon nearly in mountainous area and basin, while in early morning in plain. The diurnal maximum of PWV appears earlier in mountainous region than in plain.