Using MNRA and the monitored data of daily streamflow and meteorological factors (including precipitation, evaporation, wind speed, water vapor pressure and relative humidity) from 2003 to 2012, we determined the daily, monthly, and yearly variations in baseflow from ChangLe River watershed, a typical rainy agricultural watershed in eastern China.
We specifically analyze temperature, water vapor, all wind components, and maximum backscatter coefficients that determine the brightness of noctilucent clouds as seen by lidars.
The system registered high-frequency (20 Hz) measurements of CO2, water vapor and wind velocity in the free atmosphere as well as additional ancillary biometeorological variables (1/60 Hz) such as air temperature, solar radiation, soil heat flux, precipitation, and others.
Thus, we investigated the impact of each environmental factor by replacing water vapor, horizontal wind, or potential temperature in the initial conditions of #004-007_025 withoseofe of #007.
The last six columns show the results of a series of experiments in which the initial conditions were produced by combining the initial conditions of #004 and #007 with different weights and by replacing water vapor, horizontal wind, or potential temperature in the initial conditions of #004-007_025 withethe corresponding values of #007.
The physician Alexander Seitz, who wrote a pox treatise on demand for Elisabeth Schott, the abbess of a nunnery close to his hometown of Marbach, related this phenomenon to the idea to be found in Galen's writings according to which pain was some kind of material substance: "A back-and-forth moving pain," he explained, "is nothing other than a vapor or wind, according to Galen".
Wong, S. et al. Closing the global water budget with AIRS water vapor, MERRA winds, and evaporation, and TRMM precipitation.
In his Meteorology, Descartes described his general hypothesis about the nature of matter, before continuing on to provide accounts of vapors, salt, winds, clouds, snow, rain, hail, lightning, the rainbow, coronas, and parhelia.
Factors that affect the rate of evapotranspiration include the amount of solar radiation, atmospheric vapor pressure, temperature, wind, and soil moisture.
Besides the vegetation dynamics (V) quantified by the NDVI data, the other forcing data of this algorithm include air temperature (T) and vapor pressure (H), wind speed (W), surface radiation fluxes (R), and atmospheric CO2 concentration (C).
