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ix | |
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xix | |
Preface |
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xxi | |
Acknowledgments |
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xxix | |
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1 The definition of time and different time systems |
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1 | (18) |
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1.1 Reminder - geocentric and geographic coordinates - angle of incidence |
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2 | (3) |
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1.2 Orbit of the Earth around the sun - distance between the sun and the Earth |
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5 | (2) |
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7 | (2) |
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1.4 Definitions of time: from year to second |
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9 | (4) |
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1.4.1 Year - astronomical season - month - week |
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10 | (2) |
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1.4.2 Day - hour - minute - second |
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12 | (1) |
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1.5 Mean solar time - true solar time |
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13 | (2) |
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1.6 Coordinated universal time and legal time |
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15 | (4) |
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1.6.1 Coordinated universal time (UTC) |
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15 | (1) |
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1.6.2 Legal time - civil time - time zone |
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16 | (2) |
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1.6.3 To sum up: converting the legal time to the true solar time |
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18 | (1) |
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2 The course of the sun over an observer on the ground |
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19 | (21) |
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2.1 Position of the sun seen by an observer on the ground |
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21 | (5) |
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2.1.1 Solar zenithal angle - solar elevation - azimuth |
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22 | (3) |
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2.1.2 Direction of the sun in the case of an inclined plane |
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25 | (1) |
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2.2 Solar zenithal angles at solar noon during a year |
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26 | (1) |
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2.3 Times of sunrise and sunset |
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27 | (3) |
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30 | (1) |
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2.5 Solar angles during equinoxes and solstices |
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31 | (5) |
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2.6 Effective solar angles |
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36 | (4) |
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2.6.1 Methods for computing effective angles |
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37 | (1) |
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2.6.2 How to practically use one of these methods |
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38 | (2) |
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3 Solar radiation incident at the top of the atmosphere |
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40 | (20) |
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3.1 Radiance - irradiance - irradiation |
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41 | (4) |
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41 | (1) |
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42 | (1) |
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3.1.3 Irradiation - radiant exposure |
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43 | (1) |
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3.1.4 Converting irradiance to irradiation and vice versa |
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44 | (1) |
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3.2 Solar activity - extraterrestrial radiation |
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45 | (1) |
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3.3 Extraterrestrial radiation received on a horizontal plane |
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46 | (7) |
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3.3.1 Typical values of hourly extraterrestrial total radiation |
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47 | (4) |
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3.3.2 Daily extraterrestrial radiation |
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51 | (2) |
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3.4 Extraterrestrial radiation received on an inclined plane |
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53 | (3) |
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3.5 Spectral distribution of the extraterrestrial radiation |
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56 | (4) |
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4 Radiative transfer in the atmosphere |
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60 | (22) |
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4.1 Absorption by gases in the atmosphere |
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61 | (3) |
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4.2 Scattering - overview - case of the air molecules |
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64 | (3) |
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4.3 Attenuation - extinction |
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67 | (1) |
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4.4 Quantities related to the attenuation |
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67 | (5) |
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67 | (1) |
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4.4.2 Optical depth - optical thickness |
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68 | (1) |
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69 | (1) |
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4.4.4 Linke turbidity factor |
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70 | (1) |
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71 | (1) |
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4.5 Effects of aerosols on radiation |
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72 | (4) |
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4.6 Effects of clouds on radiation |
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76 | (2) |
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4.7 The paths of the sun rays in the atmosphere |
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78 | (2) |
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4.8 Summary of contributions of atmospheric constituents to attenuation of radiation |
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80 | (2) |
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82 | (13) |
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5.1 Reflection factor - its spectral variations |
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83 | (3) |
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83 | (2) |
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5.1.2 Examples of spectra of reflection factor |
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85 | (1) |
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5.2 Bidirectional reflectance distribution function (BRDF) |
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86 | (2) |
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88 | (7) |
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6 Solar radiation received at ground level |
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95 | (22) |
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6.1 Components of the solar radiation at ground level |
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96 | (4) |
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6.1.1 Direct, diffuse, and reflected components - global radiation |
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96 | (2) |
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6.1.2 Several definitions of the direct component |
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98 | (2) |
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6.1.3 Diffuse fraction - direct fraction |
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100 | (1) |
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100 | (6) |
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100 | (2) |
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6.2.2 An example of 15-min clearness indices |
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102 | (2) |
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6.2.3 An example of monthly clearness indices |
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104 | (2) |
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106 | (2) |
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6.4 The prominent role of clouds |
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108 | (4) |
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6.4.1 An example of hourly radiation over the North Atlantic Ocean |
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108 | (1) |
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6.4.2 Map of a multi-year average of the total solar irradiance at ground |
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109 | (3) |
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112 | (1) |
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6.6 The most important variables for the solar radiation at ground |
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112 | (2) |
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6.7 Decoupling the effects of clear atmosphere and clouds |
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114 | (3) |
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7 Spectra] distribution of the solar radiation at ground |
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117 | (15) |
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7.1 Spectral distribution of the irradiance in a cloud-free atmosphere |
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119 | (7) |
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7.1.1 Influence of the turbidity |
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119 | (2) |
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7.1.2 Spectral distribution of the direct and diffuse components |
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121 | (2) |
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7.1.3 Influence of the solar zenithal angle |
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123 | (1) |
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7.1.4 Typical irradiances integrated over some spectral intervals in a clear atmosphere |
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124 | (2) |
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7.2 Spectral distribution of the irradiance in a cloudy atmosphere |
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126 | (6) |
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7.2.1 Influence of the cloud optical depth |
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126 | (2) |
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7.2.2 Influence of the solar zenithal angle |
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128 | (1) |
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7.2.3 Typical irradiances integrated over spectral intervals in cloudy conditions |
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129 | (3) |
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8 Variability - implications for estimating radiation |
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132 | (18) |
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8.1 Time and space scales |
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133 | (3) |
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8.2 Random nature of meteorological variables - ergodicity |
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136 | (3) |
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8.3 Fluctuations around the average - small-scale variability |
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139 | (5) |
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8.4 Measurement - sampling |
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144 | (3) |
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8.5 Sampling theorem - detection of the smallest details |
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147 | (3) |
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147 | (1) |
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8.5.2 What are the smallest observable details in a series of measurements? |
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148 | (2) |
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9 Ground-based instruments for measuring solar radiation at ground |
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150 | (19) |
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9.1 Common ground-based instruments |
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152 | (5) |
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9.1.1 Thermopiles and photodiodes - calibration and classes of instruments |
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152 | (1) |
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9.1.2 Pyranometer - pyrheliometer - pyranometer with a shadow ring or ball |
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153 | (2) |
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9.1.3 Other instruments measuring global radiation and its diffuse component simultaneously |
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155 | (2) |
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9.2 Typical uncertainties of pyranometers andpyrheliometers |
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157 | (2) |
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9.3 Incomplete coverage in both space and time by stations |
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159 | (3) |
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9.4 Calculation of daily, monthly, and yearly sums and averages |
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162 | (7) |
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9.4.1 Ideal case of a complete time series of measurements |
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162 | (2) |
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9.4.2 Calculation of climate normals in meteorology |
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164 | (1) |
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9.4.3 Case of incomplete time series |
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165 | (2) |
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9.4.4 Overview of the completion of a time series |
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167 | (2) |
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10 Other means for estimating solar radiation at surface |
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169 | (20) |
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10.1 Meteorological analyses and reanalyses |
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170 | (2) |
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70.2 Images acquired by Earth observing satellites |
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172 | (7) |
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10.2.1 Multispectral imagery |
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173 | (1) |
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10.2.2 Orbits of satellites |
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174 | (2) |
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10.2.3 Overview of the methods for estimating the solar radiation |
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176 | (3) |
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10.3 Estimate using nearby ground stations |
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179 | (2) |
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10.4 Usual approach to estimate components from the only knowledge of global radiation |
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181 | (2) |
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10.5 Methods using other meteorological variables |
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183 | (6) |
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10.5.1 Angstrom's relationship between irradiation and sunshine duration |
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183 | (2) |
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10.5.2 Relationships between the total radiation and that in a given spectral range |
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185 | (1) |
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10.5.3 Estimate using other meteorological variables |
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186 | (3) |
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11 Control of the plausibility of measurements |
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189 | (18) |
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11.1 Objective of the control of plausibility |
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190 | (3) |
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11.2 How to control the plausibility of measurements |
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193 | (3) |
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11.3 Checking metadata: an overview |
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196 | (1) |
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11.4 Checking metadata: geographic location of the station |
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197 | (1) |
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11.5 Checking metadata: time system and time stamp |
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198 | (5) |
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11.5.1 Overview of the most common problems |
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198 | (3) |
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11.5.2 Some graphs for the visual inspection of the time-related problems |
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201 | (1) |
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11.5.3 Benefit in using the hourly extraterrestrial irradiation |
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202 | (1) |
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11.6 Checking metadata: checking the measured quantity and its unit |
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203 | (4) |
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12 Visual and automated procedures |
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207 | (24) |
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12.1 The principle of visual inspection |
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208 | (1) |
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12.2 Visual inspection of daily measurements |
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208 | (6) |
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12.2.1 Daily and monthly total irradiation |
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209 | (4) |
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12.2.2 An example of visual control of daily spectral values |
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213 | (1) |
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12.3 Visual inspection of hourly and intra-hourly values |
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214 | (3) |
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12.4 Two-dimensional representation of hourly and intra-hourly values |
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217 | (5) |
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12.5 Automatic procedures |
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222 | (9) |
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12.5.1 Hourly and intra-hourly measurements |
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224 | (1) |
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12.5.2 Daily measurements |
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225 | (1) |
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12.5.3 Monthly measurements |
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226 | (2) |
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12.5.4 Spectral radiation measurements |
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228 | (3) |
Index |
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231 | |