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Journal articles on the topic 'Evapo transpiration'

Author: Grafiati

Published: 3 June 2025

Last updated: 31 July 2025

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1

HARIHARAAYAR, P. S., and B. PADMANABHAMURTHY. "Water losses from an irrigated wheat field at Poona in relation to Pan Evaporation." MAUSAM 19, no. 1 (2022): 81–82. http://dx.doi.org/10.54302/mausam.v19i1.5221.

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The loss of water due evapo-transpiration from an irrigated wheat field at Poona, measured directly by the gravimetric method on a dally bass is compared with the loss of water from a standard U.S.A. pan evaporimeter. The comparison has been done by taking cumulative totals. It is seen that the two sets of values lie on a fairly smooth curve but that the ratios between the two vary considerably with the stage of growth of the crop. An attempt has been made to express the relationship between evapotranspiration and pan evaporation in a mathematical form. The study also brings out the large evap

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2

Murthy, B. S., R. Latha, Manoj Kumar, and N. C. Mahanti. "Effect of aerosols on evapo-transpiration." Atmospheric Environment 89 (June 2014): 109–18. http://dx.doi.org/10.1016/j.atmosenv.2014.02.029.

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3

Ramesh Singh, H. C. Sharma, and Ambrish Kumar. "Neuro-Fuzzy Modelling of Reference Evapo-transpiration." Journal of Agricultural Engineering (India) 45, no. 4 (2008): 23–28. http://dx.doi.org/10.52151/jae2008454.1347.

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Reference evapo-transpiration (ETo) can be either directly estimated using lysimeter or water balance approach, or estimated indirectly using the climatological data. However, it is not always possible to obtain ETo value using lysimeter, as it is a time consuming method and needs precise and carefully planned experiments. Owing to the difficulty of obtaining accurate field measurements, reference evapo-transpiration is generally estimated from weather parameters. The FA0 Penman-Monteith method has now been accepted as standard method to estimate reference evapo-transpiration. However, it requ

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4

OHNO, Tomoko, Satoshi YAMAMOTO, and Hisayuki MAENAKA. "Evapo-transpiration from Sedum Mat and Cynodon Turf." Journal of The Japanese Institute of Landscape Architecture 69, no. 5 (2006): 431–36. http://dx.doi.org/10.5632/jila.69.431.

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5

Boundi, Abdelhaq, and Zehor Ait Yacine. "Characterization of climate impacts on a semi-arid agricultural perimeter in Morocco." E3S Web of Conferences 337 (2022): 02001. http://dx.doi.org/10.1051/e3sconf/202233702001.

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The manifestations of climate change in precipitation, air temperature and simulated evapotranspiration for crops in the Tadla perimeter in central Morocco are examined. The study area is characterized by a semi-arid climate, with a potential agricultural vocation. This area is exposed to a scarcity of water resources for crop irrigation. To this effect, it is it is treating of rainfall in this area over 60 years (1958-2018) at 27 measuring stations and for temperature and reference evapo-transpiration (ETo) over 49 years (1969-2018) at 4 stations. Following data analysis by homogeneity tests

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K.C., J. K., S. Dhaubanjar, V. P. Pandey, and R. Subedi. "Water balance component analysis of a spring catchment of western Nepal." Banko Janakari 31, no. 1 (2021): 23–32. http://dx.doi.org/10.3126/banko.v31i1.37341.

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Springs in the mountains and hills are getting affected by both climatic and non-climatic changes. Hydrologic models are used to simulate the response of spring systems to the changes; however, only a limited number of studies using the hydrologic modeling approach have been accomplished on studying springs and spring-dominated watersheds in Nepal. This research aimed at understanding changing hydrological processes through hydrologic modeling in a spring catchment. A micro-catchment named 'Sikharpur' of West Seti watershed of Nepal was selected to get insights into the process influencing the

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7

Hubbard, KG. "Climatic factors that limit daily evapo-transpiration in sorghum." Climate Research 2 (1992): 73–80. http://dx.doi.org/10.3354/cr002073.

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8

Adeogun, A. G., E. O. Adeyemi, and H. O. Ganiyu. "GIS-based prediction and comparative analysis of potential evapotranspiration using selected methods at Omi-Kampe Watershed, Nigeria." Nigerian Journal of Technology 41, no. 2 (2022): 396–407. http://dx.doi.org/10.4314/njt.v41i2.22.

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The study predicted potential evapo-transpiration (PET) of Omi Kampe watershed upstream in Kogi State, Nigeria using Soil and Water Assessment Tool (SWAT) based on Priestley Taylor, Penman Monteith and Hargreaves methods. The model input data used were Digital Elevation Model, Soil map, Land use map and 30-year temporal weather data (January 1987- December 2016) for the simulation of the hydrological processes. The results showed that Penman Monteith and Hargreaves methods exhibited high correlation in the predicted values of PET while Priestley Taylor results for PET are least correlated with

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9

Sutanto, Samuel Jonson. "Global Transpiration Fraction Derived From Water Isotopologue Datasets." JURNAL TEKNIK HIDRAULIK 6, no. 2 (2018): 131–46. http://dx.doi.org/10.32679/jth.v6i2.520.

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Transpirasi sebagai salah satu komponen dari evapo-transpirasi memberikan kontribusi aliran masa yang besar dari permukaan tanah. Banyak metode telah di aplikasikan untuk menghitung besarnya komponen-komponen evapotranspirasi ini. Sebagian besar kajian dilakukan pada skala lokal maupun regional dan hanya ada sedikit kajian yang menghitung besarnya transpirasi secara global. Transpirasi global yang dihitung baik dengan model maupun dengan teknik isotop menghasilkan nilai transpirasi yang rendah untuk model dan tinggi untuk teknik isotop dibandingkan dengan pengukuran. Hal ini mengindikasikan ba

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10

Shrivastava, P., G. Rajput, and A. Pandey. "Studies on Influence of Emitter Discharge Rate, Irrigation Supplies and Planting Pattern on Tomato in Heavy Soils Of Central India." Cercetari Agronomice in Moldova 45, no. 1 (2012): 47–58. http://dx.doi.org/10.2478/v10298-012-0004-y.

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Studies on Influence of Emitter Discharge Rate, Irrigation Supplies and Planting Pattern on Tomato in Heavy Soils Of Central IndiaField experiments were conducted during two post rainy seasons at J.N. Krishi Vishwa Vidyalaya, Jabalpur, India, to evaluate the effect of emitter discharge rate, drip irrigation supplies and planting pattern on soil moisture distribution patterns and yield of tomato in heavy soils. In the experiments during 1998, irrigation was applied through emitters (2, 4 lhr-1) and micro-tubes (6 lhr-1) to conventional and paired-row plantings of tomato (var. ACC - 99). While,

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11

HASSAN, HASSANA, NATIQ AZAKI, and HALA ISSA. "A method to calculate evaporation and evapo- transpiration in Iraq." MAUSAM 38, no. 1 (1987): 103–6. http://dx.doi.org/10.54302/mausam.v38i1.2811.

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A method is presented to calculate potential evapotranspiration (PE), free surface water evaporation (E0) and pan evaporation (EPAN). The values of these parameters obtained show highly significant correlation and good agreement with the available actual measurements, The values obtained for these parameters by other different empirical formulae are found to be higher than the actual measurements.

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12

Qinglei Yang, Qing Yang, Jinli Zhang, and Jinyu Li. "Moisture Transport Simulation of Evapo-transpiration Covers with Different Initial Conditions." Journal of Convergence Information Technology 6, no. 4 (2011): 135–44. http://dx.doi.org/10.4156/jcit.vol6.issue4.16.

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13

Mahmoud Shehab, Fatin, Raid Rafi Omar, and Radhwan Yousif Sedik. "Estimating Reference Evapo- transpiration in Mosul (Iraq) Using Cascade Neural Networks." Engineering and Technology Journal 32, no. 9 (2014): 2277–85. http://dx.doi.org/10.30684/etj.32.9a14.

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14

Munavalli, G. R., and P. S. Saler. "Treatment of dairy wastewater by water hyacinth." Water Science and Technology 59, no. 4 (2009): 713–22. http://dx.doi.org/10.2166/wst.2009.008.

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The present study addresses potential of water hyacinth for treating small-scale dairy wastewater to satisfy effluent standards for disposal into public sewers. The batch experiments were conducted on dairy wastewater using reactor with water hyacinth and without water hyacinth. The Chemical Oxygen Demand (COD) was varied from 507 mg/L to 4,672 mg/L and the maximum Hydraulic Retention Time (HRT) adopted was 8 days. The loss of water due to evapo-transpiration and evaporation was also measured. The water hyacinth system performed better when initial COD concentration was maintained less than 1,

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15

Aliku, OrevaOghene, and Suarau Odutola Oshunsanya. "Modelling Irrigation Water Requirements at Physiological Growth Stages of Okra Life Cycle Using CROPWAT Model for Derived Savannah and Humid Forest Zones of Nigeria." Agricultura Tropica et Subtropica 49, no. 1-4 (2016): 20–29. http://dx.doi.org/10.1515/ats-2016-0003.

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Abstract Accurate quantification of irrigation water requirement at different physiological growth stages of okra (Abelmoschus esculentus L.) life cycle is important to prevent over or under irrigation. Field experiments were therefore initiated to model okra irrigation water requirements at the four physiological growth stages of okra life cycle using CROPWAT model. Derived savannah 1 (DS1), derived savannah 2 (DS2) and humid forest (HF) occupying 493.36 ha, 69.83 ha and 305.25 ha respectively were used. Some selected soil physical properties coupled with weather parameters were used to devel

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16

Moges, S. A., Z. Katambara, and K. Bashar. "Decision support system for estimation of potential evapo-transpiration in Pangani Basin." Physics and Chemistry of the Earth, Parts A/B/C 28, no. 20-27 (2003): 927–34. http://dx.doi.org/10.1016/j.pce.2003.08.038.

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17

Roupsard, Olivier, Jean-Marc Bonnefond, Mark Irvine, et al. "Partitioning energy and evapo-transpiration above and below a tropical palm canopy." Agricultural and Forest Meteorology 139, no. 3-4 (2006): 252–68. http://dx.doi.org/10.1016/j.agrformet.2006.07.006.

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18

Persaud, N., D. Lesolle, X. Zhou, H. Wang, and W. Joshua. "Coefficients for Penman-based estimation of daily potential evapo-transpiration in Botswana." Journal of Arid Environments 66, no. 4 (2006): 764–72. http://dx.doi.org/10.1016/j.jaridenv.2005.12.006.

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19

P. NALAYINI, R. RAJA, and ANDERSON A. KUMAR. "Evapo-transpiration based scheduling of irrigation through drip for cotton (Gossypium hirsutum)." Indian Journal of Agronomy 51, no. 3 (2001): 232–35. http://dx.doi.org/10.59797/ija.v51i3.5016.

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A field experiment was conducted during the winter season of 2001-02 and 2002-03 and summer season of 2002 and 2003 at Coimbatore, to find out the water requirement and water saving due to irrigation scheduling based on evapotranspiration (ET) through drip system compared to conventional irrigation for upland cotton (Gossypium hirsutum L.) crop. Scheduling of irrigation through drip at 0.8 Etc (crop evapotranspiration) was on a par with 1.0 Etc through drip. The total water requirement was 426.5 mm for winter crop and 467.3 mm for sum- mer crop at 0.8 Etc compared to 902.8 mm and 1,002 mm, res

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20

Alok K. Sikka, D.C. Sahoo, M. Madhu, and V. Selvi. "Determination of Crop Coefficient of Tea." Journal of Agricultural Engineering (India) 46, no. 3 (2009): 41–45. http://dx.doi.org/10.52151/jae2009463.1384.

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Crop coefficient of tea was determined based on evapo-transpiration data (1996-2001) using weighing type lysimeter. Weekly reference crop evapotranspiration (ETo) was worked out for the same period by FAO Penman–Monteith (FAO 56-PM) equation using daily meteorological data. This ETo, along with observed crop evapotranspiration (ETc), was used to determine the crop coefficient (Kc). The average Kc values for the initial season, mid season and late season were found to be 0.80, 1.31 and 0.71, respectively with the corresponding average ETc of 2.77, 3.31 and 2.27 mm/day, respectively.

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21

Kim, Byung-Sik, Jang-Hyun Sung, Hyun-Suk Kang, and Chun-Ho Cho. "Assessment of Drought Severity over South Korea using Standardized Precipitation Evapo-transpiration Index (SPEI)." Journal of Korea Water Resources Association 45, no. 9 (2012): 887–900. http://dx.doi.org/10.3741/jkwra.2012.45.9.887.

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22

Gibson, R. E., M. H. Goldsworthy, and A. M. Chandler. "Differential evapo-transpiration from a clay surface and its influence on equilibrium porewater pressure." Géotechnique 35, no. 2 (1985): 181–91. http://dx.doi.org/10.1680/geot.1985.35.2.181.

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23

Pirkner, M., U. Dicken, R. Rosa, and J. Tanny. "PERFORMANCE OF PENMAN-MONTEITH MODELS IN PREDICTING EVAPO-TRANSPIRATION IN A LARGE BANANA SCREENHOUSE." Acta Horticulturae, no. 1037 (May 2014): 353–60. http://dx.doi.org/10.17660/actahortic.2014.1037.43.

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24

Gibson, R. E., M. H. Goldsworthy, and A. M. Chandler. "Differential evapo-transpiration from a clay surface and its influence on equilibrium porewater pressure." International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts 22, no. 6 (1985): 188. http://dx.doi.org/10.1016/0148-9062(85)90176-7.

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25

Xianqun, Xie. "ESTIMATION OF DAILY EVAPO-TRANSPIRATION （ET）FROM ONE TIME-OF-DAY REMOTELY SENSEDCANOPY TEMPERATURE." National Remote Sensing Bulletin, no. 4 (1991): 253–60. http://dx.doi.org/10.11834/jrs.1991042.

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26

Hoek van Dijke, Anne J., Kaniska Mallick, Adriaan J. Teuling, et al. "Does the Normalized Difference Vegetation Index explain spatial and temporal variability in sap velocity in temperate forest ecosystems?" Hydrology and Earth System Sciences 23, no. 4 (2019): 2077–91. http://dx.doi.org/10.5194/hess-23-2077-2019.

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Abstract. Understanding the link between vegetation characteristics and tree transpiration is a critical need to facilitate satellite-based transpiration estimation. Many studies use the Normalized Difference Vegetation Index (NDVI), a proxy for tree biophysical characteristics, to estimate evapotranspiration. In this study, we investigated the link between sap velocity and 30 m resolution Landsat-derived NDVI for 20 days during 2 contrasting precipitation years in a temperate deciduous forest catchment. Sap velocity was measured in the Attert catchment in Luxembourg in 25 plots of 20×20 m cov

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27

GOURANGA KAR, ASHWANI KUMAR, and RAJBIR SINGH. "Farm level water footprints of rice production based on measured and estimated crop evapo-transpiration." Journal of Agrometeorology 16, no. 2 (2014): 157–63. http://dx.doi.org/10.54386/jam.v16i2.1506.

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Studies have been conducted to quantify water footprint (WF) on high spatial scale in which crop evapo-transpiration (ETc) was computed indirectly using empirical formula. In this study attempt has been made to quantify field level W F of rice production (varieties: ‘Lalat’ and ‘Gayatri’) in eastern India based on measured ETc. The measured values were compared with other 3 methods like Pan Evaporimeter, Bowen ratio and Penman Monteith methods. Based on measured field water balance study, 562 and 688 mm of ETc were recorded for ‘Lalat’ and ‘Gayatri’ varieties, respectively and water footprints

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28

Watanabe, Kunio, Yutaka Morita, Motoo Fujita, and Madani KEITA. "Field Measurement of Evapo-Transpiration in the Sahele Area of Republic of Mali, West Africa." Journal of the Japan Society of Engineering Geology 37, no. 2 (1996): 115–24. http://dx.doi.org/10.5110/jjseg.37.115.

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29

HIGASHI, Hironori, and Taro OKA. "A STUDY ON EVAPO-TRANSPIRATION AND SOIL MOISTURE MOVEMENT CONSIDERING PLANT GROWTH AND SAP FLOW." PROCEEDINGS OF HYDRAULIC ENGINEERING 46 (2002): 55–60. http://dx.doi.org/10.2208/prohe.46.55.

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30

Hess, T. M. "Trends in reference evapo-transpiration in the North East Arid Zone of Nigeria, 1961–91." Journal of Arid Environments 38, no. 1 (1998): 99–115. http://dx.doi.org/10.1006/jare.1997.0327.

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31

Cleverly, James R., Clifford N. Dahm, James R. Thibault, David J. Gilroy, and Julie E. Allred Coonrod. "Seasonal estimates of actual evapo-transpiration from Tamarix ramosissima stands using three-dimensional eddy covariance." Journal of Arid Environments 52, no. 2 (2002): 181–97. http://dx.doi.org/10.1006/jare.2002.0972.

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32

Van Leeuwen, Cornelis, Olivier Lerich, Romain Renard, Olivier Trégoat, and Pierre-Luc Alla. "Micromorphometric changes in trunk diameter in relation to mild water stress in field grown vines." OENO One 34, no. 2 (2000): 41. http://dx.doi.org/10.20870/oeno-one.2000.34.2.1009.

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<p style="text-align: justify;">Continuous measurement of micro variations in the diameter of woody organs provides an early detection of mild water deficits in field grown vines. Trunk diameter variations gives more reliable data than cane diameter variations. Water deficit induces trunk shrinkage and increases the Daily Contraction Amplitude / Potential Evapo Transpiration ratio ( DCA / PET). This does not occur on irrigated control vines. Moreover, micromorphometry appears to be an accurate technique for detecting short-term water deficits, because the measurements are continuous. Maj

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33

Angell, Raymond F., and Richard F. Miller. "Simulation of Leaf Conductance and Transpiration in Juniperus occidentalis." Forest Science 40, no. 1 (1994): 5–17. http://dx.doi.org/10.1093/forestscience/40.1.5.

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Abstract Western juniper (Juniperus occidentalis Hook.) is a conifer species well adapted to semiarid rangelands in portions of the western United States. Over a 2-yr period (1983-1984), water relations of mature western juniper trees were observed and soil temperature, soil water, air temperature, vapor density deficit (Da), and solar radiation were recorded. Data from 1983 were used to develop and calibrate a leaf conductance model for western juniper. The model was then tested against 1984 data. A daily soil water budget was maintained by coupling the conductance model with the hydrology co

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34

Parvathi, K. S*, Lakshmi B. S. Shubha, Arjun3 K, and B. Patil Shivakumar. "A STUDY ON CROP WATER REQUIREMENT FROM THE MANUAL METHOD." GLOBAL JOURNAL OF ENGINEERING SCIENCE AND RESEARCHES 4, no. 6 (2017): 80–84. https://doi.org/10.5281/zenodo.820354.

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The total quantity of water required by a crop from the instant of sowing till it comes to harvesting is known as water requirement of crop. Crop water requirements are normally expressed by the rate of evapo transpiration (ET) in mm day-1. From an agricultural point of view, ET determines the amount of water to be applied through artificial means. The water required for the crops from field preparation to its harvest using available data with penman method using <em>FAO 56, FAO 25, FAO 24</em> The area taken for the study is Hunasagi. Hunasagi is a village in the Shorapur taluk of Yadgir dist

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35

GOURANGA KAR and ASHWANI KUMAR. "Radiation utilization efficiency and evaporative fraction of rainfed rice in eastern India." Journal of Agrometeorology 18, no. 2 (2016): 184–89. http://dx.doi.org/10.54386/jam.v18i2.933.

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Optimum utilization of photosynthetically active radiation (PAR) along with proper nitrogen management for sustainable rice production is still a promising management recommendation in order to increase profit for the low income rice farmers of the eastern India. The objective of this investigation was to relate the cumulative development of above ground dry biomass to cumulative absorbed photosynthetically active radiation (APAR) of 2 rainfed rice varieties (‘Lalat’ and ‘Gayatri’) with 3 nitrogen levels (50, 100 and 130 kg ha-1) under tropical monsoon climate of the region. Averaged over yeas

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36

Zigene, Zewdinesh Damtew. "Physiological Studies in Horticultural Crops -An Overview." Global Academic Journal of Agriculture and Biosciences 5, no. 05 (2023): 113–24. http://dx.doi.org/10.36348/gajab.2023.v05i05.002.

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Plant physiology is the science which is connected to the material and energy exchange, growth and development, as well as movement of plant. The field of crop physiology includes the study of all the internal activities of crop plants, which are studied at many levels in the scale of size and time. Physiological study in horticultural crops like other crops, involves the basic and practically useful studies on processes such as water and nutrients in plant, nutrient supply of plants, production of primary and secondary metabolites, photosynthesis, respiration, transpiration, evapo-transpirati

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37

Parmar, Sanjaykumar H., and Mukesh K. Tiwari. "Estimation of Reference and Crop Evapo-Transpiration in Panam Canal Command using Remote Sensing and GIS." International Journal of Current Microbiology and Applied Sciences 9, no. 8 (2020): 2141–51. http://dx.doi.org/10.20546/ijcmas.2020.908.244.

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38

El-Nashar, Walaa Y., and Eman A. Hussien. "Estimating the potential evapo-transpiration and crop coefficient from climatic data in Middle Delta of Egypt." Alexandria Engineering Journal 52, no. 1 (2013): 35–42. http://dx.doi.org/10.1016/j.aej.2012.12.001.

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39

Elmi, Giovanni, Elisa Sacchi, Gian Maria Zuppi, Marcello Cerasuolo, and Enrico Allais. "Isotopic estimation of the evapo-transpiration flux in a plain agricultural region (Po plain, Northern Italy)." Applied Geochemistry 34 (July 2013): 53–64. http://dx.doi.org/10.1016/j.apgeochem.2012.12.010.

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40

Kalthoff, N., M. Fiebig-Wittmaack, C. Meißner, et al. "The energy balance, evapo-transpiration and nocturnal dew deposition of an arid valley in the Andes." Journal of Arid Environments 65, no. 3 (2006): 420–43. http://dx.doi.org/10.1016/j.jaridenv.2005.08.013.

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41

Zhou, Zhen Min, Yan Jie Bi, and Xue Chao Wang. "Improved Swat Model and Application in Simulation of Snowmelt Runoff." Advanced Materials Research 550-553 (July 2012): 2561–64. http://dx.doi.org/10.4028/www.scientific.net/amr.550-553.2561.

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The improved model for double layer snowpack melting was put forward to overcome the disadvantages of the DG (Degree-Day) model which had simple principle and neglected the relevant factors which could be important to the simulation of snowmelt runoff. The surface snowpack model, improved top layer snowpack model and model parameters calculation were studied. The structure and calculation method were put forward to improve double layer snowpack runoff model. Finally, taking the Lancangjiang River as an example, the snowmelt runoff was calculated by the improved SWAT model. Through comparison,

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42

J.I., Nirmal Kumar, Shamiyan R. Khan, Rita N. Kumar, and P. R. Sajish. "Assessment of Hydrochemical Characters Variations in Relation to Phytoplankton during Pre-monsoon at J-point of Mahi Estuary, Gujarat, India." Our Nature 11, no. 2 (2014): 85–95. http://dx.doi.org/10.3126/on.v11i2.9533.

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Variations of hydro-chemical characters were recorded at three sites of Mahi estuary, near J-point (Lat. 22º10.3′N and Long. 72º44.28′E) during the pre-monsoon period. The concentration of the nutrients was relatively high due to the elevated atmospheric temperature, evapo-transpiration of water, slow saline intrusion as well as low inflow of surface water from Mahi River. On the contrary, dissolved oxygen (DO) was at its minimum level during this investigated period. The trophic status of all the three study stations was determined in terms of DO, phosphate, nitrate and sulphate in relation t

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43

Chowdhry, Muhammad Aslam, Mohsin Ali, Ghulam Mahboob Subhani, and Ihsan Khaliq. "Path Coefficient Analysis for Water Use Efficiency, Evapo-transpiration Efficiency and Some Yield Related Traits in Wheat." Pakistan Journal of Biological Sciences 3, no. 2 (2000): 313–17. http://dx.doi.org/10.3923/pjbs.2000.313.317.

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44

Singh, K. B. "Effect of Variability in Climate and Irrigation Regimes on Evapo-transpiration and Water Use in Spring Maize." Journal of Krishi Vigyan 4, no. 1 (2015): 18. http://dx.doi.org/10.5958/2349-4433.2015.00053.7.

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45

SHIMOMURA, Takashi. "Effect of Growing Media on Growth and Evapo-transpiration after Watering Stop of Container-grown Wederia trilobata." Journal of the Japanese Institute of Landscape Architecture 58, no. 5 (1994): 89–92. http://dx.doi.org/10.5632/jila.58.5_89.

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46

Kimura, R., L. Bai, J. Fan, N. Takayama, and O. Hinokidani. "Evapo-transpiration estimation over the river basin of the Loess Plateau of China based on remote sensing." Journal of Arid Environments 68, no. 1 (2007): 53–65. http://dx.doi.org/10.1016/j.jaridenv.2006.03.029.

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47

Egwuonwu, C.C., V.C. Okafor, N.C. Ezeanya, C. Nzediegwu, and O.O. Okorafor. "A Comparison of the Reliability of Six Evapo-transpiration Computing Models for Abeokuta in South Western Nigeria." Greener Journal of Physical Sciences 2, no. 3 (2012): 64–69. https://doi.org/10.5281/zenodo.3440807.

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<strong>The Penman modified, Priestly Taylor, Blaney Morin Nigeria, Jensen-Haise, Hargreaves-Samani: and Thornthwaite methods were used to estimate Reference Evapotranspiration (RET) in Abeokuta, Ogun State Nigeria. The Penman modified method was selected as the standard of comparison for evaluating the other five methods. Good correlation was found between the RET values, estimated by each of the five radiation and temperature base and the Penman modified method, although there were some differences.</strong> <strong>The methods that performed best in estimating Penman modified RET value

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TAHASHILDAR, MOUTUSI, PRADIP K. BORA, LALA I. P. RAY, and VISHRAM RAM. "Crop-coefficients of tomato as derived using monolithic weighing type lysimeter in mid hill region of Meghalaya." MAUSAM 68, no. 4 (2021): 723–32. http://dx.doi.org/10.54302/mausam.v68i4.790.

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Crop coefficients (kc) was determined for tomato (Lycopersicon esculentum Mill.) with the help of UMS-GmBH cylindrical field lysimeter of 30 cm diameter and 120 cm deep and Penman-Monteith FAO-56 model. Eight other models viz. Modified Penman Method, Hargreaves equation, Samani-Hargreaves equation, Thornthwaite equation, Solar Radiation Method, Net Radiation Method, Blaney-Criddle Method and Radiation Method were also used for estimation of ET0 and compared with Penman-Monteith model to find out the accuracy of prediction with limited weather parameters. Scatter plot and paired t-test were us

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Amhmmed Anbeeh Albaqoul, Allam Musbah Al Allam, Waleed Ahmoda, and Tülay Ekemen KeSkin. "Meteorological and hydrological drought analysis of Sinop, Kastamonu, Bartın provinces in the Western Black Sea." مجلة جامعة بني وليد للعلوم الإنسانية والتطبيقية 8, no. 3 (2023): 80–92. http://dx.doi.org/10.58916/jhas.v8i3.118.

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In recent years, a significant change has been observed in the climate characteristics of Turkey. These changes, which are compatible with the general trend of global climate change, are also felt in the Western Black Sea Basin. This paper reported on the calculation of drought indices, with emphasis on two recently developed indices, the Reconnaissance Drought Index (RDI) and the Stream flow Drought Index (SDI) using specialized software package, named Drin C (Drought Indices Calculator). Additionally, Drin C includes a module for the estimation of potential evapo transpiration (PET) through

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Saeed, Amjad, Tanveer Hussain, Anum Choudry, et al. "Biochemical changes in Conocarpus species under saline soils of Lal Suhanra National Park, Bahawalpur." Pakistan Journal of Biochemistry and Biotechnology 2, no. 2 (2021): 207–18. http://dx.doi.org/10.52700/pjbb.v2i2.85.

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In Pakistan, arid and semi-arid areas are more prone to limited rainfall, extensive evapo-transpiration and higher temperatures. For better understandings of current situation, a field experiment was carried out to study the morphological characteristics, biochemical responses and ionic composition of Conocarpus species (Conocarpus erectus and Conocarpus lancifolius) under saline soil conditions in Lal Suhanra National Park, Bahawalpur during 2019-21. Three sites one at normal soil (S.I) and two at different salinity levels (Medium and High Salinity) were observed in order to assess their effe

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