Elsevier

Renewable Energy

Volume 36, Issue 4, April 2011, Pages 1214-1220
Renewable Energy

Estimation of solar radiation over Cambodia from long-term satellite data

https://doi.org/10.1016/j.renene.2010.09.023Get rights and content

Abstract

In this work, monthly average daily global solar irradiation over Cambodia was estimated from a long-term satellite data. A 14-year period (1995–2008) of visible channel data from GMS5, GOES9 and MTSAT-1R satellites were used to provide earth-atmospheric reflectivity. A satellite-based solar radiation model developed for a tropical environment was used to estimate surface solar radiation. The model relates the satellite-derived earth-atmospheric reflectivity to absorption and scattering coefficients of various atmospheric constituents. The absorption of solar radiation due to water vapour was calculated from precipitable water derived from ambient relative humidity and temperature. Ozone data from the TOMS and OMI satellite data were employed to compute the solar radiation absorption by ozone. The depletion of radiation due to aerosols was estimated from the visibility data. Five new solar radiation measuring stations were established at Cambodian cities, namely Siem Reap (13.87°N, 103.85°E), Kompong Thom (12.68°N, 104.88°E), Phnom Penh (11.55°N, 104.83°E), Sihanouke Ville (10.67°N, 103.63°E) and Kampot (10.70°N, 104.28°E). Global solar radiation measured at these stations was used to validate the model. The validation was also carried out by using solar radiation measured at four Thai meteorological stations. These stations are situated near the Cambodian border. Monthly average daily global irradiation from these stations was compared with that calculated from the model. The measured and calculated irradiation is in good agreement, with the root mean square difference of 6.3%, with respect to the mean values. After the validation, the model was used to calculate monthly average daily global solar irradiation over Cambodia. Based on this satellite-derived irradiation, solar radiation maps for Cambodia were generated. These maps show that solar radiation climate of this country is strongly influenced by the monsoons. A solar radiation database was also generated for solar energy applications in Cambodia.

Introduction

The amount of solar radiation incident on the earth’s surface is an important information for designing solar energy systems such as solar cells, solar water heaters and solar crop dryers as well as solar passive systems. As solar radiation has diurnal, seasonal and inter-annual variations, long-term solar radiation data are usually required for solar energy system design. Ideally, solar radiation data from the measurements at the site where the systems are intended to build should be used for designing solar energy systems. However, in reality, such data are usually not available and the radiation data from the nearest solar radiation measuring station are employed. An accurate system design is obtained if the density of the measuring stations is high enough to detect the spatial variation of solar radiation. Due to equipment and maintenance costs, the numbers and density of the stations in developing countries are usually far too low to provide sufficient solar radiation data. As an alternative, satellite data can be used to derive solar radiation data, with a reasonable accuracy, especially for a long-term average global radiation. In the past 20 years, a number of satellite-based solar radiation models have been developed with a variety of complexities and accuracies [1], [2], [3], [4], [5], [6], [7], [8], [9], [10], [11], [12], [13], [14], [15], [16], [17], [18], [19], [20], [21], [22], [23], [24], [25], [26], [27], [28], [29], [30].

For the case of Cambodia, there is great demand of solar radiation data for solar energy applications, however, there is no systematic solar radiation measurement in this country. Therefore, in this work we proposed to generate solar radiation data from long-term satellite data by using a satellite-based radiation model and five solar radiation measuring stations were established for validation of the model and for long-term systematic radiation measurement in this country.

Section snippets

Preparation of satellite data

A 14-year period of 8 bit digital hourly data taken at 8:30, 9:30, 10:30, 11:30, 12:30, 13:30, 14:30 and 15:30 h local time from the visible channel of 3 geostationary satellites namely, GMS5 (June, 1995–May, 2003), GOES9 (June, 2003–July, 2005) and MTSAT-1R (August, 2005–December, 2008), were used in this work. These data displayed as image cover the entire area of Cambodia with a spatial resolution of 3 × 3 km2. These images originally in satellite projection were transformed to the cylindrical

Description of the satellite-based radiation model

The model used in this work was originally developed for estimating solar radiation over the tropical western Pacific Ocean [12]. Then it was modified and applied for the tropical environment of Thailand [15]. The model was again improved to account for the upwelling aerosol absorption and effect of the terrain height [29]. This version was selected for this work, because it performed well for several tropical regions especially in South-east Asia. The description of this version is described

Validation of the model

As prior to this work there is no systematic solar radiation measurement in Cambodia, we established five new solar radiation measuring stations at 5 Cambodian cities, namely Siem Reap (13.87°N, 103.85°E), Kompong Thom (12.68°N, 104.88°E), Phnom Penh (11.55°N, 104.83°E), Sihanouke Ville (10.67°N, 103.63°E) and Kampot (10.70°N, 104.28°E). Global solar radiation was measured by Kipp&Zonen (CM11) pyranometers and solar radiation measured at these stations for the period: September, 2007–December,

Results and discussion

A 14-year period (1995–2008) of satellite and ancillary data were used to derive monthly average daily global irradiation. For each month, values of this irradiation were again averaged over the period of 14 years to obtain long-term average daily irradiation. The results were displayed as maps showing geographical distribution of monthly average daily solar irradiation over the country (Fig. 5). The yearly average of daily global irradiation maps is shown in Fig. 6.

From monthly solar radiation

Conclusion

A satellite-based model has been used to estimate monthly average daily global solar irradiation in Cambodia. Long-term observations of ground-based meteorological data and the satellite data for period between June, 1995 and December, 2008 were used as input of the model. Parameterization of the model considers reflection of clouds, absorption and scattering of solar radiation due to aerosols, ozone, water vapour, and gases. The earth-atmospheric reflectivity and ground albedo were estimated

Acknowledgments

The authors are grateful to the Department of Alternative Energy Development and Efficiency, Ministry of Energy of Thailand for inviting Silpakorn University to carry out this project and the permission to publish this work. The authors are also grateful to HE. Dr. Sat Samy, Deputy General Directorate, Ministry of Industry Mines and Energy of Cambodia for supporting this collaboration project. The authors would like to thank Mr. Toch Sovanna, Mr. So Veasna from the Department of Energy

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