Daily global solar radiation mapping of Turkey using Meteosat satellite data

Peştemalci, V.; Lu, Naimeng

doi:10.1080/01431160310001618743

Cited by 22 publications

(7 citation statements)

References 12 publications

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“…Furthermore, sometimes R S measurements with error up to 25% are observed due to calibration uncertainties especially when using pyranometers (Justus et al 1986;Kandirmaz et al 2004). The sources of error in measuring R S include equipment technical failure, equipment maintenance issues, and other operation-related problems (Moradi et al 2009).…”

Section: Which Need Validation Based Onmentioning

confidence: 98%

Validation and calibration of solar radiation equations for estimating daily reference evapotranspiration at cool semi-arid and arid locations

Tabari

Hosseinzadehtalaei

Willems

et al. 2015

Hydrological Sciences Journal

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In this work, the applicability of twelve solar radiation (R S ) estimation models and their impacts on daily reference evapotranspiration (ET o ) estimates using the Penman-Monteith FAO-56 (PMF-56) method were tested under cool arid and semi-arid conditions in Iran. The results indicated that the average increase in accuracy of the ET o estimates by the calibrated R S models, quantified by the decrease of RMSE, was 2.8% and 6.4% for semi-arid and arid climates, respectively. Mean daily deviations in the estimated ET o by the calibrated R S equations in semi-arid climates varied from -0.283 mm/day for the Glower-McCulloch model to 0.080 mm/day for the El-Sebaii model, with an average of -0.109 mm/day. For arid climates, mean daily deviations in the estimated ET o by the calibrated R S equations ranged from -0.522 mm/day for the Samani model to 0.668 mm/day for the El-Sebaii model, with an average of 0.125 mm/day.

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Section: Which Need Validation Based Onmentioning

confidence: 98%

Validation and calibration of solar radiation equations for estimating daily reference evapotranspiration at cool semi-arid and arid locations

Tabari

Hosseinzadehtalaei

Willems

et al. 2015

Hydrological Sciences Journal

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“…A variety of projects over the past decade have examined the use of geostationary satellite data to study aspects of solar radiation over coral reefs (Tovar and Baldasano, 2001;Hansen et al, 2002;Kandirmaz et al, 2004). organic material (Manzello et al, 2006).…”

Section: Solar Radiation and Coral Bleachingmentioning

confidence: 99%

Monitoring Coral Reefs from Space

Eakin¹,

Nim²,

Brainard³

et al. 2010

Oceanog.

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“…Some models of solar radiation computation use satellite information as input. Examples are the Heliosat family of models (Rigollier, Lefevre, and Wald 2004;Lefevre, Wald, and Diabate 2007;Moradi et al 2009), the SUNNY model (Vignola et al 2007), and other models (see for instance Kandirmaz et al 2004;Wloczyk and Richter 2006;Houborg et al 2007; for a review, see Polo, Zarzalejo, and Ramírez 2008). A simple model to estimate the daily global sunshine duration from Meteosat C3D visible type images was proposed in Kandirmaz (2006).…”

Section: Introductionmentioning

confidence: 98%

Solar Radiation Estimation From Cloudiness Data. Satellite Vs. Ground-Based Observations

Badescu

2014

International Journal of Green Energy

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Solar radiation is estimated from ground-based observations of point cloudiness C and hourly cloud fraction n data provided by Meteosat satellites. Two types of clear sky/overcast sky are defined, associated to C = 0/1 and n = 0/1, respectively. The number of hours on n-clear sky is three times larger than on C-clear sky. On C-overcast skies, the regression relationships for solar global irradiance are slightly more accurate than those for clearness index. The average irradiance on C-overcast sky is about a quarter of that on C-clear sky. The average irradiance on n-overcast sky is about one-third of that on n-clear sky.

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Daily global solar radiation mapping of Turkey using Meteosat satellite data

Cited by 22 publications

References 12 publications

Validation and calibration of solar radiation equations for estimating daily reference evapotranspiration at cool semi-arid and arid locations

Validation and calibration of solar radiation equations for estimating daily reference evapotranspiration at cool semi-arid and arid locations

Monitoring Coral Reefs from Space

Solar Radiation Estimation From Cloudiness Data. Satellite Vs. Ground-Based Observations

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