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E-grāmata: Fundamentals of Solar Radiation [Taylor & Francis e-book]

(MINES ParisTech, France)
  • Formāts: 240 pages, 17 Tables, black and white; 76 Line drawings, black and white; 27 Halftones, black and white; 103 Illustrations, black and white
  • Izdošanas datums: 12-May-2021
  • Izdevniecība: CRC Press
  • ISBN-13: 9781003155454
  • Taylor & Francis e-book
  • Cena: 222,34 €*
  • * this price gives unlimited concurrent access for unlimited time
  • Standarta cena: 317,63 €
  • Ietaupiet 30%
  • Formāts: 240 pages, 17 Tables, black and white; 76 Line drawings, black and white; 27 Halftones, black and white; 103 Illustrations, black and white
  • Izdošanas datums: 12-May-2021
  • Izdevniecība: CRC Press
  • ISBN-13: 9781003155454

The sun radiates a tremendous amount of energy, called solar energy or solar radiation, which is the main natural source of energy on the Earth, by far. Because solar radiation is the almost unique supplier of energy to the Earth, it has a primary influence on life and activities on the Earth. The climate is a first example, but there are many others, such as plant growth or human health, or even the design of buildings, the production of energy, notably electrical and thermal, or even aging materials. This book aims to provide simple answers to anyone who has questions about solar radiation. Its ambition is to help by presenting the fundamental elements of the solar radiation received on the ground. The book includes many examples and numerous illustrations, as well as some simple but fairly precise equations to calculate the various elements covered and to reproduce the figures and graphs.

The first of the three parts of this book is devoted to the relative geometry between the direction of the sun and an observer on the ground as well as to the solar radiation emitted by the sun and received at the top of the atmosphere. The orbit of the Earth around the sun and the solar declination are described. The concept of time is introduced which is closely linked to the solar cycle and the rotation of the Earth on itself. Equations are given to calculate the solar radiation received on a horizontal or inclined surface located at the top of the atmosphere. The spectral distribution of the extraterrestrial solar radiation is described. The second part of this book addresses how the solar radiation incident at the top of the atmosphere is attenuated and modified in its downward path to the ground. The reflection of the radiation by the ground is presented. The solar radiation received on the ground by a horizontal or inclined collector plane, such as a natural slope or a rooftop, is discussed, as well as its spectral distribution. The variability of the radiation is addressed in relation to the properties of solar radiation estimated from the measurements. The third part deals with direct or indirect measurements of the solar radiation received on the ground over a given integration time (minute, hour, day, or month), whether for total radiation or radiation in a spectral range such as ultraviolet (UV), or daylight, or photosynthetically active radiation (PAR). It also explains how to check the plausibility of the measurements.

Fundamentals of Solar Radiation

will be a valuable resource to all professionals, engineers, researchers, students, and other practitioners that seek an understanding of solar radiation.

List of figures
ix
List of tables
xix
Preface xxi
Acknowledgments xxix
1 The definition of time and different time systems
1(18)
1.1 Reminder - geocentric and geographic coordinates - angle of incidence
2(3)
1.2 Orbit of the Earth around the sun - distance between the sun and the Earth
5(2)
1.3 Solar declination
7(2)
1.4 Definitions of time: from year to second
9(4)
1.4.1 Year - astronomical season - month - week
10(2)
1.4.2 Day - hour - minute - second
12(1)
1.5 Mean solar time - true solar time
13(2)
1.6 Coordinated universal time and legal time
15(4)
1.6.1 Coordinated universal time (UTC)
15(1)
1.6.2 Legal time - civil time - time zone
16(2)
1.6.3 To sum up: converting the legal time to the true solar time
18(1)
2 The course of the sun over an observer on the ground
19(21)
2.1 Position of the sun seen by an observer on the ground
21(5)
2.1.1 Solar zenithal angle - solar elevation - azimuth
22(3)
2.1.2 Direction of the sun in the case of an inclined plane
25(1)
2.2 Solar zenithal angles at solar noon during a year
26(1)
2.3 Times of sunrise and sunset
27(3)
2.4 Daytime - day length
30(1)
2.5 Solar angles during equinoxes and solstices
31(5)
2.6 Effective solar angles
36(4)
2.6.1 Methods for computing effective angles
37(1)
2.6.2 How to practically use one of these methods
38(2)
3 Solar radiation incident at the top of the atmosphere
40(20)
3.1 Radiance - irradiance - irradiation
41(4)
3.1.1 Radiance
41(1)
3.1.2 Irradiance
42(1)
3.1.3 Irradiation - radiant exposure
43(1)
3.1.4 Converting irradiance to irradiation and vice versa
44(1)
3.2 Solar activity - extraterrestrial radiation
45(1)
3.3 Extraterrestrial radiation received on a horizontal plane
46(7)
3.3.1 Typical values of hourly extraterrestrial total radiation
47(4)
3.3.2 Daily extraterrestrial radiation
51(2)
3.4 Extraterrestrial radiation received on an inclined plane
53(3)
3.5 Spectral distribution of the extraterrestrial radiation
56(4)
4 Radiative transfer in the atmosphere
60(22)
4.1 Absorption by gases in the atmosphere
61(3)
4.2 Scattering - overview - case of the air molecules
64(3)
4.3 Attenuation - extinction
67(1)
4.4 Quantities related to the attenuation
67(5)
4.4.1 Air mass
67(1)
4.4.2 Optical depth - optical thickness
68(1)
4.4.3 Transmittance
69(1)
4.4.4 Linke turbidity factor
70(1)
4.4.5 Visibility
71(1)
4.5 Effects of aerosols on radiation
72(4)
4.6 Effects of clouds on radiation
76(2)
4.7 The paths of the sun rays in the atmosphere
78(2)
4.8 Summary of contributions of atmospheric constituents to attenuation of radiation
80(2)
5 Ground reflection
82(13)
5.1 Reflection factor - its spectral variations
83(3)
5.1.1 Reflection factor
83(2)
5.1.2 Examples of spectra of reflection factor
85(1)
5.2 Bidirectional reflectance distribution function (BRDF)
86(2)
5.3 Albedo
88(7)
6 Solar radiation received at ground level
95(22)
6.1 Components of the solar radiation at ground level
96(4)
6.1.1 Direct, diffuse, and reflected components - global radiation
96(2)
6.1.2 Several definitions of the direct component
98(2)
6.1.3 Diffuse fraction - direct fraction
100(1)
6.2 Clearness index
100(6)
6.2.1 Definition
100(2)
6.2.2 An example of 15-min clearness indices
102(2)
6.2.3 An example of monthly clearness indices
104(2)
6.3 Clear-sky index
106(2)
6.4 The prominent role of clouds
108(4)
6.4.1 An example of hourly radiation over the North Atlantic Ocean
108(1)
6.4.2 Map of a multi-year average of the total solar irradiance at ground
109(3)
6.5 Sunshine duration
112(1)
6.6 The most important variables for the solar radiation at ground
112(2)
6.7 Decoupling the effects of clear atmosphere and clouds
114(3)
7 Spectra] distribution of the solar radiation at ground
117(15)
7.1 Spectral distribution of the irradiance in a cloud-free atmosphere
119(7)
7.1.1 Influence of the turbidity
119(2)
7.1.2 Spectral distribution of the direct and diffuse components
121(2)
7.1.3 Influence of the solar zenithal angle
123(1)
7.1.4 Typical irradiances integrated over some spectral intervals in a clear atmosphere
124(2)
7.2 Spectral distribution of the irradiance in a cloudy atmosphere
126(6)
7.2.1 Influence of the cloud optical depth
126(2)
7.2.2 Influence of the solar zenithal angle
128(1)
7.2.3 Typical irradiances integrated over spectral intervals in cloudy conditions
129(3)
8 Variability - implications for estimating radiation
132(18)
8.1 Time and space scales
133(3)
8.2 Random nature of meteorological variables - ergodicity
136(3)
8.3 Fluctuations around the average - small-scale variability
139(5)
8.4 Measurement - sampling
144(3)
8.5 Sampling theorem - detection of the smallest details
147(3)
8.5.1 Sampling theorem
147(1)
8.5.2 What are the smallest observable details in a series of measurements?
148(2)
9 Ground-based instruments for measuring solar radiation at ground
150(19)
9.1 Common ground-based instruments
152(5)
9.1.1 Thermopiles and photodiodes - calibration and classes of instruments
152(1)
9.1.2 Pyranometer - pyrheliometer - pyranometer with a shadow ring or ball
153(2)
9.1.3 Other instruments measuring global radiation and its diffuse component simultaneously
155(2)
9.2 Typical uncertainties of pyranometers andpyrheliometers
157(2)
9.3 Incomplete coverage in both space and time by stations
159(3)
9.4 Calculation of daily, monthly, and yearly sums and averages
162(7)
9.4.1 Ideal case of a complete time series of measurements
162(2)
9.4.2 Calculation of climate normals in meteorology
164(1)
9.4.3 Case of incomplete time series
165(2)
9.4.4 Overview of the completion of a time series
167(2)
10 Other means for estimating solar radiation at surface
169(20)
10.1 Meteorological analyses and reanalyses
170(2)
70.2 Images acquired by Earth observing satellites
172(7)
10.2.1 Multispectral imagery
173(1)
10.2.2 Orbits of satellites
174(2)
10.2.3 Overview of the methods for estimating the solar radiation
176(3)
10.3 Estimate using nearby ground stations
179(2)
10.4 Usual approach to estimate components from the only knowledge of global radiation
181(2)
10.5 Methods using other meteorological variables
183(6)
10.5.1 Angstrom's relationship between irradiation and sunshine duration
183(2)
10.5.2 Relationships between the total radiation and that in a given spectral range
185(1)
10.5.3 Estimate using other meteorological variables
186(3)
11 Control of the plausibility of measurements
189(18)
11.1 Objective of the control of plausibility
190(3)
11.2 How to control the plausibility of measurements
193(3)
11.3 Checking metadata: an overview
196(1)
11.4 Checking metadata: geographic location of the station
197(1)
11.5 Checking metadata: time system and time stamp
198(5)
11.5.1 Overview of the most common problems
198(3)
11.5.2 Some graphs for the visual inspection of the time-related problems
201(1)
11.5.3 Benefit in using the hourly extraterrestrial irradiation
202(1)
11.6 Checking metadata: checking the measured quantity and its unit
203(4)
12 Visual and automated procedures
207(24)
12.1 The principle of visual inspection
208(1)
12.2 Visual inspection of daily measurements
208(6)
12.2.1 Daily and monthly total irradiation
209(4)
12.2.2 An example of visual control of daily spectral values
213(1)
12.3 Visual inspection of hourly and intra-hourly values
214(3)
12.4 Two-dimensional representation of hourly and intra-hourly values
217(5)
12.5 Automatic procedures
222(9)
12.5.1 Hourly and intra-hourly measurements
224(1)
12.5.2 Daily measurements
225(1)
12.5.3 Monthly measurements
226(2)
12.5.4 Spectral radiation measurements
228(3)
Index 231
Lucien Wald received the M.S. degree in theoretical physics in Marseille and Paris, France, in 1977, the Ph.D. degree from the University UPMC, Paris, in 1980, and the Doctorat dEtat čs Sciences on the applications of remote sensing to oceanography from the University in Toulon, France, in 1985. Since 1991, he has been a Professor at the MINES ParisTech. He created a research team and was its head till 2007. He was responsible of PhD studies in energy from 2005 to 2012. He retired in 2018. Lucien Wald contributed to the birth and progress of Earth observation. He has been very active within the European association of remote sensing laboratories (EARSeL) from 1980 to 2009, and then within the European Meteorological Society (EMS). His activities in data science were rewarded in 1996 with the famous French Blondel Medal. He was the recipient of the Autometrics Award in 1998 and the Erdas Award in 2001 from the American Society for Photogrammetry and Remote Sensing for articles on data fusion. His other research activities focused mainly on geosciences: oceanography, meteorology and solar radiation. His scientific publications cover Earth observation, marine, terrestrial and urban environments, air pollution, meteorology, solar radiation and its effects on human health. Lucien Wald on Publons. https://publons.com/researcher/2863398/lucien-wald/metrics/ Lucien Wald on Google citations. https://scholar.google.fr/citations?user=hRxJ0zAAAAAJ&hl=fr