DOI: https://doi.org/10.36995/j.recyt.2025.43.001
Improving
the efficiency of photovoltaic generation by adapting to meteorological
elements
Mejora de la eficiencia de la generación fotovoltaica
adaptándose a los elementos meteorológicos
Melhoria da eficiência da geração fotovoltaica por
meio da adaptação aos elementos meteorológicos
Elisardo do Prado, Porto1, *; Cássio Aurélio, Suski1
1- Santa Catarina Federal Institute. Brazil.
* E-mail: elisardo.porto@ifsc.edu.br
Received: 01/12/2023; Accepted: 12/11/2024
Abstract
The production of clean electricity, which does not harm
environmental systems, has been one of the main global priorities in recent times. The range of ultraviolet
radiation, sent through sunlight, which can be captured by photovoltaic cells
and transformed into electrical energy, makes the sun
the most promising source to supply the electrical needs of human beings. The
climate is of considerable importance in capturing solar energy, as the
efficiency of a cell system is directly related to local climate conditions.
This paper aims to analyse the influence of
meteorological elements on the efficiency of photovoltaic energy generation and
its climatic effect. The methodology is based on
measuring the generation of electricity through
photovoltaic cells, compiling meteorological elements and panel
temperature, studying the relationship between electricity generation using
photovoltaic cells and other parameters, and surveying parameters to improve the efficiency of clean energy generation. The results
show a relationship between the generation of electricity through photovoltaic
cells and the other parameters, providing an average generation 11% higher in
wind directions between 330 and 360° at the study site, as well as enabling an
alternative to reduce of up to 5.3% of the emission of greenhouse gases through
the expansion of photovoltaic energy generation and reduction of energy
generation by hydroelectric and thermoelectric plants, which are currently
positioned as the largest sources in Brazil.
Keywords: Photovoltaic,
Solar energy, Climate and environment, Meteorological elements, Greenhouse
gases.
Resumen
La producción de
electricidad limpia que no dañe los sistemas medioambientales ha sido una de
las principales carreras mundiales de los últimos tiempos. Los niveles de
radiación ultravioleta, enviada a través de la luz solar, que pueden ser
captadas por células fotovoltaicas y transformar la luz en energía eléctrica,
hacen del sol la fuente más prometedora para satisfacer las necesidades
eléctricas de los seres humanos. El clima tiene una importancia considerable a
la hora de captar energía solar, ya que la eficiencia de un sistema celular
está directamente relacionada con las condiciones climáticas locales. Este
trabajo tiene como objetivo analizar la influencia de los elementos
meteorológicos en la eficiencia de la generación de energía fotovoltaica y su efecto
climático. La metodología se basa en la medición de la generación de
electricidad mediante celdas fotovoltaicas, en la recopilación de elementos
meteorológicos y temperatura del panel; en el estudio de la relación entre la
generación de electricidad mediante células fotovoltaicas y el resto de
parámetros y en el estudio de los parámetros para la mejora de la eficiencia de
la generación de energía limpia. Los resultados muestran una relación entre la
generación de electricidad a través de células fotovoltaicas y el resto de
parámetros, proporcionando una generación promedio un 11% mayor en direcciones
del viento entre 330 y 360° en el sitio de estudio, además de permitir una
alternativa de reducción de hasta 5,3 % de la emisión de gases de efecto invernadero
a través de la expansión de la generación de energía fotovoltaica y la
reducción de la generación de energía por centrales hidroeléctricas y
termoeléctricas, que actualmente se posicionan como las mayores fuentes de
Brasil.
Palabras clave: Fotovoltaica, Energía
solar, Clima y medio ambiente, Elementos meteorológicos, Gases de efecto
invernadero.
Resumo
A produção de
eletricidade limpa, que não agride os sistemas ambientais, tem sido uma das
principais corridas globais dos últimos tempos. As faixas de radiação
ultravioleta, enviadas através da luz solar, que podem ser captadas pelas
células fotovoltaicas e transformar a luz em energia elétrica, fazem do sol a
fonte mais promissora para suprir as necessidades elétricas do ser humano. O
clima tem considerável importância na captação de energia solar, pois a
eficiência de um sistema celular está diretamente relacionada às condições
climáticas locais. Este artigo tem como objetivo analisar a influência dos
elementos meteorológicos na eficiência da geração de energia fotovoltaica e seu
efeito climático. A metodologia baseia-se na medição da geração de energia
elétrica por meio de células fotovoltaicas, na compilação de elementos
meteorológicos e temperatura do painel; no estudo da relação entre a geração de
energia elétrica por meio de células fotovoltaicas e os demais parâmetros e no
levantamento dos parâmetros para melhoria da eficiência da geração de energia
limpa. Os resultados mostram uma relação entre a geração de energia elétrica
através de células fotovoltaicas e os demais parâmetros, proporcionando uma
geração média 11% maior nas direções do vento entre 330 e 360° no local de
estudo, além de possibilitar uma alternativa de redução de até 5,3 % da emissão
de gases de efeito estufa através da expansão da geração de energia
fotovoltaica e redução da geração de energia pelas usinas hidrelétricas e
termelétricas, que atualmente se posicionam como as maiores fontes do Brasil.
Palavras-chave: Fotovoltaica, Energia solar, Clima e meio ambiente,
Elementos meteorológicos, Gases de efeito estufa.
INTRODUCTION
Global warming and clean energy production are
important concerns related to climate and the environment. The lack of
investment, combined with the lack of information and practical projects on the
part of public authorities, justifies the slow progress in the conquest of
clean energies.
The increase in global temperature is
exacerbated by anthropogenic actions that disrupt the planet's natural
greenhouse effect, primarily due to rising greenhouse gas emissions. This is
caused by the burning of fossil fuels in thermoelectric plants, the
decomposition of organic matter left over from the cutting of trees and the
carbon present in the soil flooded by hydroelectric plants, among other
emission sources.
The energy generated by the sun, an
inexhaustible source on the timescale of planet Earth's existence, in its two
main functions of heat and light, is undoubtedly one of the most promising
energy alternatives for providing the energy necessary for human development.
When talking about energy, it should be remembered that the sun is responsible
for the origin of virtually all other energy sources on Earth (Hayat et al., 2018).
Atmospheric factors generally observed in the
production of solar energy are cloudiness, air humidity and ambient
temperature, but the availability of solar radiation, which is the incident
energy on the earth's surface, is also influenced by the inclination of the
planet in relation to the sun that varies during the day, month and year
(ANEEL, 2008).
The duration of sunlight varies according to the
region of the planet and time of year, specifically mentioning the issue of the
solstices that occur at the North Pole, when on December 21st there may even be
no sun exposure, or on June 21st, when it can reach up to 24 hours of sun
exposure (Raza et al., 2019).
The first studies on the photovoltaic effect
were observed in 1839 and improved with the use of other materials. The first
significant advances in these studies occurred between the 1930s and 1950s of
the last century, with the development of photovoltaic cells composed of
silicon crystals, which form the basis of current cells (Wolfe, 2018).
The photoelectric effect is a physical process
of the element that converts sunlight into electrical energy, and the light
energy absorbed by the photovoltaic cell is transferred to its atoms and
electrons. These electrons are released from the component atoms of the
semiconductor material, allowing for the electric current to flow through in an
ordered manner (Hanifi et al., 2018).
Photovoltaic modules are a set of encapsulated
photovoltaic cells, whose purpose is to protect the cells from the weather,
mainly from air humidity (Kholod et al.,
2018).
Pure photovoltaic generation is one that does
not involve any other form of electricity generation. Since the system
generates electricity only during sunny hours, autonomous or off-grid systems
are equipped with accumulators that store energy for periods without sunlight,
which take place every night, and during rainy or cloudy periods. Accumulators
are batteries sized according to the autonomy of the system. Conventional
off-grid power systems for charging battery banks require a charge controller
with Maximum Power Point Tracking (MPPT) technology (Jain et al., 2021).
According to the National Electric Energy Agency
(ANEEL, 2018), Brazil has an installed solar generating plant capacity of
1,797,580 kW, which represents 1% of the total power of projects in Brazil.
However, the number of solar photovoltaic generating centres is 2,273 units,
representing approximately 32% of the total number of installed projects,
second only to thermoelectric plants.
Regarding the effective participation in the
generation of electricity in the Brazilian electrical system, solar energy has
evolved in recent years, with 5.7% in 2016, 7.2% in 2017, and 8.3% in 2018.
That is, investments in new generating units have been increasing (ANEEL,
2018).
However, according to Matin et al. (2020), only 33.33% of the light energy incident on
photovoltaic cells is absorbed for the generation of electricity; that is, the
generation efficiency of photovoltaic cells is still quite low and influenced
by temperature, solar irradiance and, consequently, by meteorological elements.
Despite this, few studies evaluate the meteorological variables that are
related to the efficiency of electric power generation.
Climatic conditions play a crucial role in solar
energy generation, as the excess or lack of specific phenomena can impact
energy capture. A climate with high humidity and no wind can generate
excessively hot conditions near the cells, which impairs energy production,
and, in addition, humidity can create precipitation and clouds that cover up
and make it difficult to absorb solar radiation. Wind is one of the key
elements, as it moves air masses, pushing moisture and clouds and cooling the
photovoltaic system (Navntoft et al.,
2019).
This
study is justified by the excellent opportunity for research work to assess the
influence of meteorological elements on the efficiency of electricity
generation by photovoltaic cells, aiming to enable the increased participation
of solar power plants in electricity generation. With this objective in mind,
among other subjects, the primary sources of electricity generation, the
respective greenhouse gas emissions and how meteorological elements can affect
the generation of energy by photovoltaic cells will be analysed.
METHODOLOGY
For
the development of research and analysis of the influence of meteorological elements
on the efficiency of electricity generation using photovoltaic cells, the study
was divided into the following stages: measurement of electricity generation
using photovoltaic cells; compilation of meteorological elements and panel
temperature; relationship between the generation of electricity through
photovoltaic cells and the other parameters, and parameters for improving the
efficiency of clean energy generation.
The study was carried out in the
city of Itajaí (Figure 1), located on
the north coast of the state of Santa Catarina (Latitude 26° 55' 51" S and
Longitude 048° 41' 05" W), on the right bank of the mouth of the
Itajaí-Açu river, in the southern region of Brazil.
Figure 1 -
Location of the Municipality of Itajaí.
Source:
Map generated from Interactive Map information - GeoSEUC / Unofficial basemap,
© OpenStreetMap contributors.
The measurement of local
electricity generation was conducted from December
2022 to April 2023. For this measurement, a solar energy generator kit with
photovoltaic cells, model CS6U-325P, manufactured by Canadian Solar, was
used. It was installed in the Northwest direction
(282° NW).
The kit was attached to the Sanches
prototype meteorological station (2020), with wind direction (HMC-5883 sensor),
wind speed (Hall sensor - US-1881), relative humidity (HDC-1080 sensor),
atmospheric pressure and temperature sensors (BMP-180), as well as UV sensors
ML8511, Type K Thermocouple Temperature Sensor of the solar cell and data
transmission via RS485 communication cable to USB with reading software
installed.
The set, comprising
mechanical and electrical-electronic structures, was installed in a free area
on a roof, approximately 12 meters above the ground.
The electro-electronic structure is
composed of an XTRA4210N-XDS2 battery charge and discharge controller and 40A
flow current with MPPT (Maximum Power Point Tracking) technology, together with
a bank of 03 Model 12MN105 batteries, the Model IP2000-22 inverter module and
the protection system with circuit breakers, earthing and lightning protection
devices.
Figure 2
demonstrates the layout scheme formed by the photovoltaic
cell system, weather station and protection devices.
Figure 2 -
Sensor installation scheme.
Source:
Author.
The power generation set was
installed and later calibrated by checking the
voltage and current at the input and output of the controller using a
multimeter (ET-1002 Minipa). This verification ensured that the voltage (37.0
V) and current (8.0 V, 78 A) were adequate, and consequently, power was generated (325
W).
The system operates off-grid (i.e., it is not connected to the official energy
distributor's network) and is connected to consumer equipment with approximately
500W of power during the entire period of energy
generation.
The reading of the generated voltage
(V), current produced (A), and calculated power
(W) was performed every 10 minutes using the XTRA4210N-XDS2 charge controller,
which is available in real time on a display and in LandStar B software (LS-B).
Subsequently, the voltage, current,
and power reading data were correlated with the
meteorological elements and panel temperature.
The meteorological station performed
readings of meteorological elements, including wind speed and direction,
relative humidity, atmospheric pressure, air temperature, UV radiation, and panel temperature, synchronised with the reading of the charge controller (electricity)
every 10 minutes.
The
meteorological station utilised an electronic prototyping platform
featuring free hardware and a single-board microcontroller (Arduino) that
employs the C++ programming language. This platform generated a database of the
parameters above.
Relationship
between the generation of electricity through photovoltaic cells and the other
parameters
After measuring and compiling the
data obtained in C++ and LS-B (Embedded) programming languages,
Table 1 was formatted, along with correlation graphs
for discussion and analysis of the influence of meteorological elements on
energy generation.
In this step, the power generated by
the panel was correlated with meteorological elements (wind speed and
direction, relative humidity, atmospheric pressure, temperature, and
ultraviolet radiation) and panel temperature to assess the efficiency of the
photovoltaic cells in generating electric energy.
Such correlations, as well as basic statistics, were obtained using Minitab,
with support from Spearman's Rho method.
Table 1 - Relationship between the generation
of electricity through photovoltaic cells and the other parameters.
|
DT |
H |
GER |
PT |
T |
RH |
UV |
WS |
WD |
AP |
|
d/m/y |
h:m:s |
W |
°C |
°C |
% |
Index |
m/s |
° |
mmHg |
Where: DT = Date, H = Time, GER =
Generation, PT = Panel Temperature, T = Ambient Temperature, RH = Relative
Humidity of Air, UV = Ultraviolet, WS = Wind Speed, WD = Wind Direction, AP =
Atmospheric Pressure,
Source:
Author.
The analysis first considered the
average generation of the four quadrants of the wind direction (WD), between 0
and 360°, of the third quartile (above 175 W of photovoltaic energy generation)
and, subsequently, it was possible to identify more specifically the wind
directions (330-360°) that had the highest mean power generation for the third
quartile.
From these data, correlations were
made between the variables wind speed, relative humidity, atmospheric pressure,
temperature, radiation (UV) and panel temperature.
Through the interpolation of the
relationship of the parameters, the hypothesis of use
was generated in relation to the installation position and the meteorological
elements to obtain the best efficiency of the
photovoltaic cells, providing the reduction of the use of electric energy
generated by hydroelectric and thermoelectric plants and, consequently,
predicting their influence on the environmental impact and the generation of
greenhouse gases (GHG).
The effect of improving the
efficiency of clean energy generation on the environment was measured through a survey of the possible reduction of hydroelectric plants
and by the decrease in fuel consumption (oil,
biomass and coal) in thermoelectric plants and, consequently, the emission of
GHG.
For the evaluation of the reduction
of GHG emissions in this study, three scenarios were proposed (Table 2), in addition to the current scenario. The scenario categorised as current is based on the percentage of electricity
generation in Brazil in 2018. The other scenarios were determined with gradual
reductions in the percentage of use of hydroelectric (hydraulic) and thermoelectric (biomass, oil and coal) plants. Based on the proposed
scenarios, GHG emission reductions were calculated using the emission
factors for each emission source.
To estimate CO2 emissions
in hydraulic, wind, natural gas, oil, coal and nuclear energy generation, the
emission factors estimated by Miranda1 (2012) were considered.
The biomass and solar emission
factors were obtained from the Low Carbon Study for Brazil2 - Land
Use, Land Use Change and Forests by Soares Filho et al. (2010) and the Covenant of Mayors for Climate and Energy3
by Neves et al. (2016), respectively
(Table 3).
For the case of energy in
hydroelectric plants, Life Cycle Assessment studies were considered that
encompass stages of construction, generation, and
emissions from reservoirs, as these have significant emissions and characterise
the operation phase of the plant. Additionally, the total installed capacity of
electricity-generating sources in Brazil is 164,187
MW.
Table 2 -
Proposed scenarios for analysis of greenhouse gas emissions (%).
|
|
Percentage of
energy generation by type of source |
||||||||
|
Scenario |
Hydraulics |
Biomass |
Wind |
Natural gas |
Oil |
Coal |
Nuclear |
Solar |
Total |
|
Current (2018) |
63.7 |
9.0 |
8.8 |
8.0 |
6.1 |
2.2 |
1.2 |
1.0 |
100 |
|
1 |
63.2 |
8.8 |
8.8 |
8.0 |
6.0 |
2.0 |
1.2 |
2.0 |
|
|
2 |
62.6 |
8.7 |
8.8 |
8.0 |
5.9 |
1.8 |
1.2 |
3.0 |
|
|
3 |
62.0 |
8.6 |
8.8 |
8.0 |
5.8 |
1.6 |
1.2 |
4.0 |
|
Source: ANEEL, 2018
Table 3 - GHG emission factors from
generation sources.
|
|
Hydraulics1 |
Biomass2 |
Wind1 |
Natural Gas1 |
Oil1 |
Coal1 |
Nuclear1 |
Solar3 |
|
Factor (gCO 2eq /kWh) |
86 |
1580 |
16 |
518 |
829 |
1144 |
14 |
50 |
Source:
Author.
The
methodology for calculating carbon emissions for energy generation sources (EGHG)
is based on the installed energy production capacity (CPLANT) and
the GHG emission factor (FGHG), and the calculation can be
represented by Equation 1:
(1)
Where:
EGHG - Estimate of GHG
generation (ton CO2eq)
CPPLANT - Installed
Energy Production Capacity (kWh)
FGHG- GHG emission factor
(gCO2eq /kWh)
To calculate the reduction in the
area of the hydroelectric reservoir due to the decrease in generation through this source, Equations 2 and 3 are used.
(2)
Where:
EGHG at - GHG generation
in hydroelectric plants for the total flooded area (ton CO2eq);
EGHG - GHG emissions ton
CO2eq per km2;
A RES CUR - Total
reservoir area in the current scenario (km2).
(3)
Where:
RARES - Reduction of hydroelectric
reservoir area (km2);
ARES CUR - Area of the
hydroelectric reservoir in the current scenario (km2);
ARES
SCEN3 - Hydroelectric reservoir area in scenario 3 (km2).
RESULTS
AND DISCUSSIONS
Figure
3 shows scatter plots between power generation and
wind direction in four different situations. One can observe the increasing
trend of generations as the wind direction approaches the fourth quadrant
(Figure 3a). By filtering the data for the third quartile of generation, that
is, where the highest generation of energy occurs, it is also possible to
perceive the increasing trend of the data (Figures 3b and 3c), which makes it
possible to observe a higher average generation of energy in the wind direction
of 330 - 360° (Figure 3d).
Table
4 shows the average energy generation (general data) of 100.18 W, and Table 5 shows the energy generation correlations with
the other parameters, with the most significant values of UV and panel
temperature, 0.483 and 0.442, respectively.
|
a.
General generation data for all WD |
b.
Generation data greater than 175 W
(third quartile) for all WD |
|
|
|
|
c.
Generation data greater than 175 W
(third quartile) for WD 270 – 360° |
d.
Generation data greater than
175 W (third quartile) for WD 300 – 360° |
|
|
|
Figure 3 -
Scatter charts with trend line.
Table 4 - Mean values (general data) of the analysed parameters.
|
GER (W) |
PT
(°C) |
T
(°C) |
RH (%) |
UV
(mW/c) |
WS
(m/s) |
WD
(°) |
AP
(mmHg) |
|
100.18 |
227.33 |
29.04 |
59.00 |
7.00 |
0.16 |
98.44 |
1,012.30 |
Table
5 - Correlations between generation and other parameters.
|
|
PT |
T |
RH |
UV |
WS |
WD |
AP |
|
Generation |
0.442 |
0.371 |
-0.338 |
0.483 |
0.068 |
0.157 |
0.044 |
|
p-value |
0.000 |
0.000 |
0.000 |
0.000 |
0.000 |
0.000 |
0.000 |
With the fractionation of the
historical series of energy generation in subsamples, using the third quartile
of the wind direction as a filter, that is, dividing 25% of the data of the
largest generations into four quadrants of wind performance, where 0 to 90°
constitute the first sample, between
90 and 180° the second sample, and so on, it is observed in Table 6 that the average power generation is 258.79 W
between 0 and 90° (first quadrant), 257.36 W in the second quadrant, 257.47 W
in the third quadrant and 270.00 W in the fourth quadrant, resulting in a slight increase in generation efficiency in the last quadrant in
relation to the other quadrants.
After
surveying the averages of electric energy generation in the third quartile in
relation to each quadrant of wind direction, the range of analysis can be
adjusted for the highest average of energy generations and, with that, it was
identified that the wind direction between 330 and 360° has the highest average
generation of the third quartile, with a value of 299.6 W (Table 7), resulting in an increase in energy generation
efficiency of approximately 11% in relation to the average of the fourth
quadrant.
Employing the
correlations (Tables 8 to 12) between the
values obtained by reading the meteorological elements and the generation data
and panel temperature, a more detailed observation of these data can be
initiated.
It can be observed that, in general,
the correlations between energy generation and wind direction, panel
temperature and ultraviolet radiation provide more significant values concerning the other elements.
Table 6 - Mean values of parameters analysed in the third quartile in relation to wind direction.
a. Generation greater than 175 W and WD between 0 and 90°
|
Variable |
N |
N* |
Average |
SE average |
Standard deviation |
Minimum |
Q1 |
Median |
Q3 |
Maximum |
|
Generation |
465 |
0 |
258.79 |
3.07 |
66.22 |
175.07 |
205.90 |
244.70 |
296.13 |
513.47 |
|
PT |
465 |
0 |
30,130 |
0.182 |
3,923 |
20,660 |
29,650 |
29,650 |
32,360 |
43,250 |
|
T |
465 |
0 |
31,163 |
0.125 |
2,685 |
20,610 |
31,790 |
31,790 |
33,330 |
41,530 |
|
RH |
465 |
0 |
51,829 |
0.438 |
9,434 |
30,240 |
50,970 |
50,970 |
51,175 |
86,800 |
|
UV |
465 |
0 |
7.2224 |
0.0262 |
0.5640 |
6.0400 |
7.1400 |
7.1400 |
7,5500 |
9.9100 |
|
WS |
465 |
0 |
0.0594 |
0.0064 |
0.1389 |
0.0000 |
0.0000 |
0.0000 |
0.1000 |
0.9100 |
|
WD |
465 |
0 |
12.13 |
1.18 |
25.50 |
0.00 |
0.00 |
0.00 |
0.00 |
90.00 |
|
AP |
465 |
0 |
1012.7 |
0.161 |
3.48 |
101.4 |
1013.5 |
1013.5 |
1015.4 |
1020.5 |
b.
Generation greater than 175 W and WD
between 90 and 180°
|
Variable |
N |
N* |
Average |
SE average |
Standard deviation |
Minimum |
Q1 |
Median |
Q3 |
Maximum |
|
Generation |
495 |
0 |
257.36 |
3.30 |
73.49 |
175.00 |
200.85 |
237.19 |
297.84 |
696.47 |
|
PT |
495 |
0 |
29,923 |
0.206 |
4,583 |
16,770 |
26,980 |
29,410 |
32,160 |
44,180 |
|
T |
495 |
0 |
30,514 |
0.143 |
3,172 |
17,240 |
28,560 |
30,710 |
32,450 |
39,920 |
|
RH |
495 |
0 |
51,900 |
0.404 |
8,978 |
26,920 |
45,330 |
51,400 |
57,970 |
79,370 |
|
UV |
495 |
0 |
7.2905 |
0.0259 |
0.5768 |
6.1300 |
6,9000 |
7,1800 |
7,6700 |
9,8700 |
|
WS |
495 |
0 |
0.1737 |
0.0072 |
0.1612 |
0.0200 |
0.0500 |
0.1200 |
0.2400 |
0.8700 |
|
WD |
495 |
0 |
148.32 |
1.14 |
25.34 |
90.00 |
129.00 |
152.00 |
170.00 |
180.00 |
|
AP |
495 |
0 |
1013.3 |
0.158 |
3.51 |
1003.6 |
1011.0 |
1013.9 |
1015.8 |
1020.4 |
c.
Generation greater than 175 W and WD
between 180 and 270°
|
Variable |
N |
N* |
Average |
SE average |
Standard deviation |
Minimum |
Q1 |
Median |
Q3 |
Maximum |
|
Generation |
238 |
0 |
257.47 |
3.95 |
60.90 |
175.12 |
206.36 |
244.71 |
297.44 |
491.49 |
|
PT |
238 |
0 |
29,350 |
0.262 |
4,049 |
16,770 |
26,488 |
29,155 |
31,595 |
40,330 |
|
T |
238 |
0 |
30,673 |
0.221 |
3,413 |
17,240 |
28,212 |
31,140 |
33,245 |
37,570 |
|
RH |
238 |
0 |
51,617 |
0.549 |
8,475 |
36,460 |
45,863 |
50,045 |
56,438 |
78,870 |
|
UV |
238 |
0 |
7.2196 |
0.0325 |
0.5015 |
5.6400 |
6.9300 |
7.1400 |
7.5200 |
9.0200 |
|
WS |
238 |
0 |
0.1441 |
0.0076 |
0.1181 |
0.0200 |
0.0500 |
0.11000 |
0.2000 |
0.5900 |
|
WD |
238 |
0 |
215.95 |
1.79 |
27.64 |
180.00 |
191.00 |
212.00 |
241.25 |
270.00 |
|
AP |
238 |
0 |
1011.5 |
0.244 |
3.76 |
1003.6 |
1008.3 |
1011.2 |
1013.9 |
1020.5 |
d. Generation greater than 175 W and WD between 270 and 360°
|
Variable |
N |
N* |
Average |
SE average |
Standard deviation |
Minimum |
Q1 |
Median |
Q3 |
Maximum |
|
Generation |
58 |
0 |
270.0 |
10.2 |
77.4 |
177.7 |
203.8 |
250.2 |
318.6 |
546.2 |
|
PT |
58 |
0 |
31,868 |
0.568 |
4,323 |
23,270 |
29,260 |
31,050 |
34,255 |
45,860 |
|
T |
58 |
0 |
32,664 |
0.416 |
3,166 |
25,250 |
31,248 |
32,475 |
34,487 |
42,290 |
|
RH |
58 |
0 |
46.16 |
1.12 |
8.53 |
31.15 |
40.45 |
44.91 |
50.54 |
73.22 |
|
UV |
58 |
0 |
7,4891 |
0.0733 |
0.5579 |
6,5700 |
7.0200 |
7.5300 |
7,8000 |
9.3400 |
|
WS |
58 |
0 |
0.1895 |
0.0210 |
0.1602 |
0.0200 |
0.0700 |
0.1450 |
0.2775 |
0.7700 |
|
WD |
58 |
0 |
315.57 |
3.21 |
24.45 |
271.00 |
296.25 |
316.00 |
334.00 |
357.00 |
|
AP |
58 |
0 |
1011.6 |
0.545 |
4.15 |
1004.4 |
1007.6 |
1012.0 |
1014.8 |
1019.9 |
Table 7 -
Mean values of parameters analysed in the third
quartile in relation to wind direction between 330 and 360°.
|
Variable |
N |
N* |
Average |
SE average |
Standard deviation |
Minimum |
Q1 |
Median |
Q3 |
Maximum |
|
Generation |
16 |
0 |
299.6 |
18.8 |
75.3 |
182.7 |
233.8 |
299.1 |
365.7 |
419.7 |
|
PT |
16 |
0 |
31,737 |
0.828 |
3,314 |
26,500 |
29,343 |
31,240 |
33,295 |
39,700 |
|
T |
16 |
0 |
33,180 |
0.898 |
3,591 |
26,600 |
30,782 |
32,285 |
35,907 |
40,730 |
|
RH |
16 |
0 |
46.09 |
2.45 |
9.81 |
34.62 |
39.17 |
06.43 |
52.23 |
72.64 |
|
UV |
16 |
0 |
7,917 |
0.160 |
0.638 |
6,940 |
7,630 |
7,755 |
8,287 |
9,340 |
|
WS |
16 |
0 |
0.2650 |
0.0542 |
0.2167 |
0.0200 |
0.1250 |
0.2100 |
0.4050 |
0.7700 |
|
WD |
16 |
0 |
346.38 |
2.00 |
8.02 |
332.00 |
341.00 |
347.00 |
354.50 |
357.00 |
|
AP |
16 |
0 |
1011.1 |
0.883 |
3.53 |
1004.4 |
1009.2 |
1012.0 |
1012.9 |
1016.4 |
In the third quadrant (Table 10), the highest correlation between ultraviolet
radiation and power generation can be found, reaching a value of 0.401,
considered moderate. There is still an inverse proportional relationship in
relation to relative humidity of -0.313. Given these numerical factors, one
can, empirically, have an impression of this being
the quadrant that presents the most positive results for the study.
However, when establishing a
correlation by observing the concentration of data with higher generation
values, it is identified that there is a range of coordinates in the northwest
direction, 330 to 360° (Table 12), which presents average values of
generation (299.6 W) that are higher (Figure 4).
Table 8 -
Correlation of 1st
wind direction quadrant (0 to 90°) and generation greater than 175 W.
|
|
PT |
T |
RH |
UV |
WS |
WD |
AP |
|
Generation |
0.308 |
0.223 |
-0.284 |
0.308 |
0.180 |
0.184 |
-0.093 |
|
p-value |
0.000 |
0.000 |
0.000 |
0.000 |
0.000 |
0.000 |
0.000 |
Table 9 - Correlation of 2nd wind direction quadrant (90 to 180°) and
generation greater than 175 W.
|
|
PT |
T |
RH |
UV |
WS |
WD |
AP |
|
Generation |
0.228 |
0.207 |
-0.181 |
0.292 |
0.063 |
-0.019 |
-0.096 |
|
p-value |
0.000 |
0.000 |
0.000 |
0.000 |
0.162 |
0.674 |
0.032 |
Table 10 - Correlation of 3rd wind direction quadrant (180 to 270°) and
generation greater than 175 W.
|
|
PT |
T |
RH |
UV |
WS |
WD |
AP |
|
Generation |
0.397 |
0.315 |
-0.313 |
0.401 |
0.132 |
0.066 |
-0.132 |
|
p-value |
0.000 |
0.000 |
0.000 |
0.000 |
0.043 |
0.314 |
0.041 |
Table 11 - Correlation of 4th wind direction quadrant (270 to 360°) and
generation greater than 175 W.
|
|
PT |
T |
RH |
UV |
WS |
WD |
AP |
|
Generation |
0.115 |
-0.018 |
0.077 |
0.253 |
0.082 |
0.333 |
-0.119 |
|
p-value |
0.392 |
0.892 |
0.567 |
0.053 |
0.540 |
0.011 |
0.375 |
Table 12 - Correlations for wind direction
(330 to 360°) and generation greater than 175 W.
|
|
PT |
T |
RH |
UV |
WS |
WD |
AP |
|
Generation |
-0.112 |
-0.271 |
0.315 |
-0.231 |
-0.021 |
0.010 |
0.253 |
|
p-value |
0.680 |
0.311 |
0.425 |
0.389 |
0.940 |
0.970 |
0.345 |
To make data analysis
more accurate, it can be observed that, in addition to the wind direction
between 330 and 360º, there is a punctual estimate for the highest average, the
lower limit for the average generation estimate, in this wind direction
interval, nearly exceeds the upper bound for the average generation estimates
for all other quadrants. The statistical test in this range rejects
equality with a p-value of 0.07, which is very close to
95% reliability.
Figure
4 - Reliability Ratio for Energy Generation.
Thus,
it can be observed that energy generation is a function of a composition of
variables, which may differ in each region or location of installation of
photovoltaic panels and, in this case in particular, higher generation occurs
in wind directions between 330 and 360°, where the panel temperature, ambient
temperature, ultraviolet radiation and wind speed are higher than in the other
directions. Atmospheric pressure is maintained in all directions, and relative humidity is lower than in other directions.
According to Matin et al. (2020), the
generation efficiency of photovoltaic cells is still relatively low and influenced by temperature and solar irradiance
and, consequently, by meteorological elements.
Such specificity may be related to
the characteristic geographic position of the observation site in the
municipality of Itajaí, where the collector side of the photovoltaic panels is
installed at 282° NW. The northwest wind is drier, originating from within the state of Santa
Catarina, leaving the sky with less cloudiness and increasing the ultraviolet
radiation, which falls within an optimal range for
energy generation.
Climatic conditions play a crucial
role in solar energy generation, as the excess or lack of certain phenomena can
directly affect energy capture. A climate characterised by high humidity and a lack
of wind can result in excessively hot conditions around solar cells,
significantly impairing energy production. Additionally, the presence of
moisture can lead to the formation of precipitation and clouds that cover and hinder the efficient absorption of solar radiation. The
wind, in turn, is an essential element, as it
has the role of moving air masses, displacing moisture and dispersing clouds.
Furthermore, it plays a crucial role in cooling the PV system, thereby contributing to its overall efficiency and performance.
According to the sensitivity
analysis conducted by LV et al.
(2014), based on solar power generation measurement data in 2011, from a
comprehensive perspective of daily and monthly power generation, the top five
climate variables of importance are solar radiation time (i.e. solar
radiation), speed wind, relative humidity, cloud cover and outside temperature.
The power generated by photovoltaic
modules is linearly dependent on irradiance, except for small values of
irradiance when the output power is zero. The efficiency of the photovoltaic
plant not only strongly depends on the irradiance, but also depends on the
module temperature (Chokmajirov et al., 2006).
In this study, no significant variations were identified between the panel temperature
and the ambient temperature (Table 6), including the average temperature of the
panel around 1°C lower than the ambient temperature. This fact may be related
to the location and position of the panel's installation, as the
photovoltaic set is elevated above the roof, allowing for air circulation and convection on the panels.
According to Hamrouni et al. (2008), for
several solar radiations ranging from 100 to 1000 W/m² and for a constant
temperature equal to 25 °C, there is an increase in generation with an increase
in radiation and a maximum global efficiency of the photovoltaic system for 300
W/m² of radiation.
According to research by Kaldellis et al. (2014), as wind speed
increases, the working temperature of photovoltaic cells gradually approaches
ambient temperature, which affects the efficiency of
power generation. Thus, the photovoltaic conversion process, in addition to
instantaneous solar radiation, also depends on the temperature of the modules.
The module temperature, in turn, is influenced by climatic conditions, as well
as by the technical characteristics of the photovoltaic panels.
Solar irradiance has the most
significant impact on the output power of a
photovoltaic system (Diaf et al., 2008). In addition to irradiance, weather conditions such
as ambient temperature, along with several other factors (e.g. angle of
incidence [AOI], dust, etc.) (Kaldellis et al., 2012)
can also affect the power output and energy production of a photovoltaic
module. To this end, the module temperature is influenced by the ambient
temperature, cloud patterns and wind speed (Buday, 2011), while the temperature change rate also depends on the PV
material and frame position.
Normally, the impact of free
convection is quite limited, while the radiation mechanism is dominant during
low wind speed values (Kaldellis et al., 2014).
The photovoltaic conversion process,
in addition to instantaneous solar radiation, also depends on the temperature
of the modules. The module temperature, in turn, depends on climatic conditions
(such as ambient temperature, solar irradiation, and wind speed) and the
technical characteristics of the photovoltaic panels (including material, type,
assembly, and ventilation) (Kaldellis et al., 2014).
For a better characterisation and prediction of photovoltaic module performance under a
wide variety of climatic conditions, several detailed studies have been carried
out (Jacques et al., 2013; Armstrong et al., 2010) and several models have
been proposed, with most of them based on only in controlled indoor
measurements (for example, controlling the wind flow over the panel surface
with fans).
Based
on the results of improving the efficiency of photovoltaic energy generation,
it is possible to perceive the potential for reducing greenhouse gas (GHG)
emissions from hydroelectric and thermoelectric plants, thereby enhancing the use of solar energy.
Tables 13 and 14 show the values of
energy generation and emissions calculated using Equation 1, by type of energy generation and for each
proposed scenario. In these scenarios, the values referring to energy related
to wind, natural gas, and nuclear were kept constant, while energy from
hydraulic and thermal power plants (biomass, coal, and oil) was reduced, and
energy from solar sources was increased.
In the current scenario, there is a
total gas emission of 28,609 x 10 6 ton CO2eq, while in
the proposed scenarios 28,170; 27,592 and 27,078 x 10 6 ton
CO2eq are generated, that is, a reduction of approximately 1,531 x
10 6 ton CO2eq in Scenario
3 compared to the current scenario, which results in a 5.3% reduction.
According to the IPCC special report
(2021), it is crucial to reduce greenhouse gas (GHG) emissions by 45% by 2030,
compared to 2010 levels, to limit the increase in global average temperature to
1.5°C above pre-industrial levels. This reduction is necessary to avoid more
serious consequences of climate change.
Although a 5.3% reduction in
emissions, related to the generation of electricity in Brazil, is not enough to
generate a significant impact on
the increase in global average temperature, it is one more factor to be
considered for mitigating global warming, and it
is fundamental to recognise that this phenomenon is complex and influenced by several
factors. Therefore, in addition to this progress, a significantly
greater effort is needed, in terms of electricity generation sources, to achieve the global warming mitigation targets
established by the IPCC and prevent significant and irreversible impacts.
Table 13 - Energy generation for each scenario
and each generation source.
|
|
Power generation (MW) |
||||||||
|
Scenario |
Hydraulics |
Biomass |
Wind |
Natural gas |
Oil |
Coal |
Nuclear |
Solar |
Total |
|
Current (2018) |
104,587 |
14,776 |
14,448 |
13,134 |
10,015 |
3,612 |
1,970 |
1,641 |
164,187 |
|
1 |
103,766 |
14,448 |
14,448 |
13,134 |
9,851 |
3,283 |
1,970 |
3,283 |
|
|
2 |
102,781 |
14,284 |
14,448 |
13,134 |
9,687 |
2,955 |
1,970 |
4,925 |
|
|
3 |
101,795 |
14,120 |
14,448 |
13,134 |
9,522 |
2,626 |
1,970 |
6,567 |
|
Table 14 - GHG emissions for each scenario.
|
|
Emissions (x 10 6 ton CO2eq) |
|
||||||||
|
Scenarios |
Hydraulics |
Biomass |
Wind |
Natural gas |
Oil |
Coal |
Nuclear |
Solar |
Total |
Reduction (%) |
|
Current (2018) |
9,016 |
12 |
233 |
6,805 |
8,302 |
4,132 |
27 |
82 |
28,609 |
- |
|
1 |
8,945 |
11 |
233 |
6,805 |
8,166 |
3,756 |
27 |
164 |
28,107 |
1.7 |
|
2 |
8,860 |
11 |
233 |
6,805 |
8,030 |
3,380 |
27 |
246 |
27,592 |
3.5 |
|
3 |
8,775 |
11 |
233 |
6,805 |
7,894 |
3,005 |
27 |
328 |
27,078 |
5.3 |
Due to the reduction in energy generation from thermoelectric
plants, there is a reduction in consumption (Table
15) of fuels (coal, oil and biomass), reaching a maximum reduction of 27% for
coal and approximately 5% for oil and biomass.
Table 15 - Reductions in fuel used in
thermoelectric plants.
|
|
Fuel consumption (kg) |
||||
|
Fuel |
Current scenario |
Scene 1 |
Scenario 2 |
Scenario 3 |
Reduction (%) Scenario 3 x Current scenario |
|
Coal |
1,242,795 |
1,129,814 |
1,016,832 |
903,851 |
27.3 |
|
Oil |
2,549,874 |
2,508,072 |
2,466,271 |
2,424,470 |
4.9 |
|
Biomass |
7,628,195 |
7,458,679 |
7,373,921 |
7,289,164 |
4.5 |
By
reducing the percentage of energy generation through hydraulic sources,
biomass, oil and coal (Table 14), maintaining
energy generation through wind, natural gas and nuclear sources and expanding
energy generation through solar source, in addition to a reduction in CO2 emissions
from the generation itself, there is also a possibility of reducing
emissions from the generation of CH4 due to the anaerobic
decomposition of organic matter present in the hydroelectric lakes (Barros et al., 2021).
Zanoni
et al.
(2015) analysed
the characteristics of the flooded soil and the CH4 production that
is produced at the bottom of the reservoirs by the anaerobic decomposition of
the organic matter and emitted in the water-air interface, through bubbles or
diffusion, demonstrating that the local
factors of the flooding influence the amount of CH4 produced.
According to some authors (Louis et al., 2000; Pueyo et al., 2011),
the average methane emission rate in hydroelectric plants can vary from 20 to
300 mg of CH4 /m² per day, depending on local conditions.
According to the method presented by
Santos et al. (2008), CH4 emission
is 18.29 kg.km-2.day -1, which corresponds to an annual
emission of 0.36 ton x 10 6 in 55,000 km² of reservoir area,
resulting in 2.06 ton x 10 6 CO 2eq year, considering a
CH4 GWP of 21.
Considering GHG generation in
Hydroelectric Power Plants for the total flooded area (EGHGatl), for
the current scenario, at 9,016 x 106 ton CO2eq (Table 14) and the total reservoir area of 55,000 km², the
GHG emission per km² (EGHG) can be calculated using Equation 2.
From the issuance of scenario 3
(8,775 x 106 ton CO2eq - Table 14), the final area of the reservoir can then be
calculated.
And, through Equation 3, it is possible to
calculate its consequent reduction in area (approximately 2.7%), due to the
reduction in energy generation through hydroelectric plants.
These equations are a simplified way
of estimating the generation of greenhouse gases in hydroelectric power plants
and, it is important to remember that the emission factor may vary according to
the characteristics of each plant and that other factors may influence emissions,
such as the type of vegetation removed during the construction of the reservoir
and the type of soil present in the region.
According to the ANEEL, there are
approximately 220 hydroelectric power plants in operation in Brazil, with a
total installed capacity of more than 104 gigawatts
(GW) as of 2022. The
ANEEL provides detailed information about each of these plants, including the
size of dams, the area flooded and the volume of water stored.
Through studies by the Ministry of
Mines and Energy of Brazil, it is possible to verify that in the year 2020
there was a significant consumption of energy from hydroelectric plants, totalling 396,381 GWh (MME, 2022). The substantial amount of
energy generated by hydroelectric plants underscores the importance of this
sector in the national energy matrix, highlighting its crucial role in
supplying electricity to the country.
However, it is worth remembering
that the hydroelectric plants in operation in Brazil have a total area of dams
of approximately 55,000 km² (ANEEL, 2022) and it is also worth noting that the
size of dams of hydroelectric plants in Brazil is subject of debate and controversy due to the
socio-environmental impacts that these undertakings cause. Several organisations and social movements have questioned the construction of
large dams, arguing that they cause the loss of forest areas, the displacement
of traditional communities, and the forced relocation
of riverside populations (Fearnside, 2020).
Amaral et al. (2019) conducted an environmental assessment of
hydroelectric power plants in Brazil, employing life cycle analysis and
inventory methodologies. Based on this, the authors
calculated greenhouse gas (GHG) emissions and other environmental impact
categories, considering the plant's power density to differentiate emissions
per km² of flooded area. The results indicated
that power density was a significant factor in determining GHG
emissions, with notable variations between the
evaluated power plants. The study emphasised the importance of considering
power density as a key factor in the environmental
assessment of hydroelectric power plants. The estimation of greenhouse
gas emissions associated with hydroelectric energy generation can be performed
using a simplified equation that considers the plant's energy generation
capacity, the reservoir area, and the emission
factor.
The works by Miranda (2012) and
Amaral (2019) address the assessment of the environmental performance of
hydroelectric power plants, focusing on the analysis of greenhouse gas (GHG)
emissions. Both studies employ the life cycle approach to assess GHG
emissions throughout the life cycle of power plants,
from construction to end of life.
While Miranda (2012) emphasises the importance of considering the plant's power density in
assessing GHG emissions, Amaral (2019) utilises this concept to
calculate GHG emissions per square kilometre of
flooded area. This approach enables a more accurate assessment of the
environmental performance of various hydroelectric plants, taking into account
the unique characteristics of each project. By
combining these approaches, it is possible to obtain a more comprehensive assessment of the environmental performance of
hydroelectric plants.
In
addition, it is essential to note that the National Electric
Energy Agency (ANEEL), in its Annual Report on the Inspection of the Use of the
Union's Heritage (2022), uses electricity generation capacity and the total
area of dams in Brazil as references to estimate
greenhouse gas emissions. This approach considers the diversity of existing
plants and dams in the country, which have different operational
characteristics and environmental impacts. However,
it is important to point out that this methodology can be improved with the
inclusion of specific emission factors for each plant, as proposed by Miranda
and Amaral.
Final
considerations
By analysing the influence of wind direction and speed, ambient
temperature, relative humidity, atmospheric pressure, ultraviolet radiation and
panel temperature on the efficiency of photovoltaic energy generation and its
climate effect, it can be identified that:
●
The efficiency of photovoltaic
energy generation can be influenced by the composition of meteorological
elements and panel temperature, and may vary in each region
or location where photovoltaic panels are installed.
●
In the specific case of this study,
there is an average generation 11% higher in wind directions between 330 and
360°, since the collector face of the photovoltaic panels is installed at 282°
NW and the northwest wind is a drier wind, coming from within the state of
Santa Catarina, leaving the sky with less cloudiness, expanding ultraviolet
radiation to within a range of excellent standards for energy generation.
●
The proposition of scenarios with an
increase in the percentage of energy generation by photovoltaic panels results
in a reduction in greenhouse gas emissions of up to 5.3%.
●
The reduction in energy generation
through hydroelectric plants, proposed in the scenarios, allows for a 2.7%
reduction in the area of the reservoirs.
●
The reduction in energy generation
through thermoelectric plants, proposed in the scenarios, makes it possible to
reduce the consumption of coal, oil and biomass by 27.3%, 4.9% and 4.5%,
respectively.
The
study provides one more factor to consider for mitigating global warming, and it is essential to recognise that this phenomenon is complex and influenced by several
components.
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