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Wang Suping - One of the best experts on this subject based on the ideXlab platform.
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Trends of Potential Evapotranspiration in Maqu County of Gansu Province in Recent 40 Years
Journal of Arid Meteorology, 2020Co-Authors: Wang SupingAbstract:Based on meteorological data during 1971-2010 from Maqu weather station,the monthly Potential Evapotranspiration was calculated by using the Penman-Monteith method,and the trends of Potential Evapotranspiration in Maqu were analyzed by using statistic analysis,Mann-Kendall method and wavelet analysis.The results indicated that the annual variation of Potential Evapotranspiration presented a significant increasing trend with the rate of 12.0 mm/10 a,and there was quasi-10 and quasi-5 years change period.The trend of pan-evaporation was similar to the Potential Evapotranspiration in Maqu.Monthly mean of the Potential Evapotranspiration presented single peak with increase from January to July and going down from August.The maximum of monthly mean Potential Evapotranspiration occurred in July.The seasonal distribution of Potential Evapotranspiration was consistent with precipitation and temperature in Maqu.
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The variety characters of Potential Evapotranspiration and soil surface humidity index in Hezuo,Gansu During 1961-2010
Journal of Arid Land Resources and Environment, 2020Co-Authors: Wang SupingAbstract:To study the variety of the Potential Evapotranspiration and the soil surface humidity index of the border area in the North-East Qinghai-Xizang plateau,the Hezuo was selected as an example site.Based on the meteorological data(1961~2010) of the Hezuo weather observation station,the Potential Evapotranspiration was computed by using Penman-Monteith model,and the changes of Potential Evapotranspiration and soil surface humidity index of Hezuo meadow was analyzed.The results indicated that the Potential Evapotranspiration in Hezuo showed an obvious increasing tendency with the tendency ratio of 13.0mm/10a;the climate tendency of soil surface humidity index was-0.02/10a,the warm-drying tendency was obviously.The most important climatic factors to the Potential Evapotranspiration increasing were the temperature and air humidity,next were the sunshine duration,precipitation and the wind speed.
Carmela Chao De Báez - One of the best experts on this subject based on the ideXlab platform.
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ESTIMATION OF Potential Evapotranspiration WITH HARGREAVES-SAMANI MODEL AT VARIOUS LOCATIONS IN PUERTO RICO
Journal of Agriculture of The University of Puerto Rico, 1991Co-Authors: Megh R. Goyal, Carmela Chao De BáezAbstract:ESTIMATION OF Potential Evapotranspiration WITH HARGREAVES-SAMANI MODEL AT VARIOUS LOCATIONS IN PUERTO RICO
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CLASS A PAN EVAPORATION VERSUS Potential Evapotranspiration AT SEVEN LOCATIONS IN PUERTO RICO
Journal of Agriculture of The University of Puerto Rico, 1990Co-Authors: Carmela Chao De Báez, Megh R. GoyalAbstract:CLASS A PAN EVAPORATION VERSUS Potential Evapotranspiration AT SEVEN LOCATIONS IN PUERTO RICO
Mohammad Valipour - One of the best experts on this subject based on the ideXlab platform.
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analysis of Potential Evapotranspiration using limited weather data
Applied Water Science, 2017Co-Authors: Mohammad ValipourAbstract:The most important weather variations are temperature (T), relative humidity (RH), and wind speed (u) for Evapotranspiration models in limited data conditions. This study aims to compare three T-based formula, T/RH-based formula, and T/RH/u-based formula to detect the performance of them under limited data and different weather conditions. For this purpose, weather data were gathered from 181 synoptic stations in 31 provinces of Iran. The Potential Evapotranspiration was compared with the FAO Penman–Monteith method. The results showed that T-based formula, T/RH-based formula, and T/RH/u-based formula estimated Potential Evapotranspiration with R 2 >0.93 for 6, 12, and 30 provinces of Iran, respectively. They are more suitable for southeast of Iran (YA, KE, SB, and SK). The best precise method was the T/RH/u-based formula for SK and GO. Finally, a list of the best performance of each method has been presented to use other regions and next researches according to values of temperature, relative humidity, and wind speed. The best weather conditions to use the formulas are 14–26 °C and 2.50–3.50 m/s for temperature and wind speed, respectively.
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evaluation of radiation methods to study Potential Evapotranspiration of 31 provinces
Meteorology and Atmospheric Physics, 2015Co-Authors: Mohammad ValipourAbstract:The present study aims to calibrate radiation-based methods to determine the best method under different weather conditions. For this purpose, weather data was collected from different synoptic stations in all of provinces of Iran. The Potential Evapotranspiration was estimated using common radiation-based methods and a sensitive analysis was done for investigating variations of the methods. The results show that the Stephens method estimates the Potential Evapotranspiration better than other methods in the most provinces of Iran (10 provinces). However, the values of R 2 were less than 0.98 for 15 provinces of Iran. The calibrated methods estimated the Potential Evapotranspiration in the south east of Iran better than other provinces. Precision of the methods calibrated has been increased in all provinces. The R 2 values are less than 0.98 for only six provinces (WA, EA, GO, NK, AL, and QO). In the methods calibrated, the Abtew (for YA) estimated the Potential Evapotranspiration better than the other methods.
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retracted comparative evaluation of radiation based methods for estimation of Potential Evapotranspiration
Journal of Hydrologic Engineering, 2015Co-Authors: Mohammad ValipourAbstract:AbstractEvapotranspiration has a major role in agricultural and forest meteorology researches, hydrological cycle, irrigation scheduling, and water resources management. There are many methods to estimate the Potential Evapotranspiration including mass transfer, radiation, temperature, and pan evaporation-based methods. The present study aims to compare radiation-based methods to determine the best method under different weather conditions. The results discussed in this paper are from the data collected in the study area, but the method can be used in other similar regions. For this purpose, weather data was collected from 181 synoptic stations in 31 provinces of Iran. The Potential Evapotranspiration was estimated using 22 radiation-based methods and compared with the Food and Agriculture Organization of the United Nations (FAO) Penman-Monteith method. The results show that the Stephens method estimates the Potential Evapotranspiration better than other methods for provinces of Iran. However, the values ...
Megh R. Goyal - One of the best experts on this subject based on the ideXlab platform.
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ESTIMATION OF Potential Evapotranspiration WITH HARGREAVES-SAMANI MODEL AT VARIOUS LOCATIONS IN PUERTO RICO
Journal of Agriculture of The University of Puerto Rico, 1991Co-Authors: Megh R. Goyal, Carmela Chao De BáezAbstract:ESTIMATION OF Potential Evapotranspiration WITH HARGREAVES-SAMANI MODEL AT VARIOUS LOCATIONS IN PUERTO RICO
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CLASS A PAN EVAPORATION VERSUS Potential Evapotranspiration AT SEVEN LOCATIONS IN PUERTO RICO
Journal of Agriculture of The University of Puerto Rico, 1990Co-Authors: Carmela Chao De Báez, Megh R. GoyalAbstract:CLASS A PAN EVAPORATION VERSUS Potential Evapotranspiration AT SEVEN LOCATIONS IN PUERTO RICO
Wang Jian-bin - One of the best experts on this subject based on the ideXlab platform.
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The Variety Characters of Potential Evapotranspiration and Soil Surface Humidity Index in the Zoige Wetland in1971-2010
2020Co-Authors: Wang Jian-binAbstract:The meteorological data of the Zoige, Hongyuan and Maqu weather observation stations were used,the Potential Evapotranspiration was computed by using Penman-Monteith model. The results indicated that the Potential Evapotranspiration variation in the Zoige wetland shows an obvious increasing tendency with the tendency ratio of 9.1 mm/10 a,An abrupt change of the Potential Evapotranspiration was detected in the 2001,the mean Potential Evapotranspiration during 2001-2010 has increased by 28.6 mm compared with that of1971-2000. The autumn Potential Evapotranspiration increased with the tendency ratio of 4.3mm/10 a,its more higher than the other seasons. The annual Potential Evapotranspiration's minimum period is 1980 s, it obviously increased from 1990 s, the variety of seasonal Potential Evapotranspiration in spring, summer and autumn is very similar to that of annual. The winter Potential Evapotranspiration minimum period is 1990 s, it obviously increased in the 21 st.The cycle change is 7-8 a during 1970 s and 1980 s, from the end of 1980 s to the end of1990 s, it is an obviously adjusted period, the cycle change is 5a from the beginning of 21 st. The temperature rising, relative humidity and precipitation decreasing are the major contributors to the Potential Evapotranspiration increased. Although the decreasing of the sunshine duration and mean wind velocity is help to the Potential Evapotranspiration decreased, but the temperature rising plays a more important role to the Potential Evapotranspiration increased. The decreasing tendency of soil surface humidity index is-0.03/10 a,the soil surface humidity index has decreased 0.11 during 2001-2010 compared with that of 1981-1990. meanwhile, the increasing tendency of the mean temperature is 0.41℃/10 a, the decreasing tendency of the precipitation is-13.5mm/10 a, the climate change of the Zoige wetland shows an obviously warm-drying tendency.