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Floating PV gallery example #2110

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2 changes: 2 additions & 0 deletions docs/examples/floating-pv/README.rst
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Floating PV Systems Modelling
-----------------------------
217 changes: 217 additions & 0 deletions docs/examples/floating-pv/plot_floating_pv_cell_temperature.py
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r"""
Calculating the cell temperature for floating PV
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================================================

This example demonstrates how to calculate the cell temperature for
floating photovoltaic (FPV) systems using the PVSyst temperature model.
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One of the primary benefits attributed to FPV systems
is lower operating temperatures, which are expected to increase the
operating efficiency. In general, the temperature at which a photovoltaic
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module operates is influenced by various factors including solar radiation,
ambient temperature, wind speed and direction, and the characteristics of the
cell and module materials, as well as the mounting structure. Both radiative
and convective heat transfers play roles in determining the module's
temperature.
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A popular model for calculating the PV cell temperature is the
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empirical heat loss factor model suggested by Faiman. A modified version of
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this model is implemented in PVSyst
(:py:func:`~pvlib.temperature.pvsyst_cell`). The PVSyst model for cell
temperature :math:`T_{C}` is given by

.. math::
:label: pvsyst

T_{C} = T_{a} + \frac{\alpha \cdot E \cdot (1 - \eta_{m})}{U_{c} + U_{v} \cdot WS}

Where :math:`E` is the plane-of-array irradiance, :math:`T_{a}` is the
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ambient air temperature, :math:`WS` is the wind speed, :math:`\alpha` is the
absorbed fraction of the incident irradiance, :math:`\eta_{m}` is the
electrical efficiency of the module, :math:`U_{c}` is the wind-idependent heat
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loss coefficient, and :math:`U_{v}` is the wind-dependent heat loss coefficient.

However, the default heat loss coefficient values of this model were
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specified for land-based PV systems and are not necessarily representative
for FPV systems.
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In FPV systems, variations in heat loss coefficients are considerable, not
only due to differences in design but also because of geographic factors.
Systems with extensive water surfaces, closely packed modules, and restricted
airflow behind the modules generally exhibit lower heat loss coefficients
compared to those with smaller water surfaces and better airflow behind the
modules.

For FPV systems installed over water without direct contact, the module's
operating temperature, much like in land-based systems, is mainly influenced
by the mounting structure (which significantly affects the U-value), wind,
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and air temperature. Thus, factors that help reduce operating temperatures in
such systems include lower air temperatures and changes in air flow beneath
the modules (wind/convection). In some designs where the modules are in
direct thermal contact with water, cooling effectiveness is largely dictated
by the water temperature.

The table below gives heat loss coefficients derrived for different systems
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and locations as found in the literature. In this example, the FPV cell
temperature will be calculated using some of the coefficients below.

+-------------------------+-------------+--------------------------------+----------------------------------------+-----------+
| System | Location |:math:`U_{c}` | :math:`U_{v}` | Reference |
| | |:math:`[\frac{W}{m^2 \cdot K}]` | :math:`[\frac{W}{m^3 \cdot K \cdot s}]`| |
+=========================+=============+================================+========================================+===========+
| Monofacial module, | Netherlands | 24.4 | 6.5 | [1]_ |
| open structure, | | | | |
| two-axis tracking, | | | | |
| small water footprint | | | | |
+-------------------------+-------------+--------------------------------+----------------------------------------+-----------+
| Monofacial module, | Netherlands | 25.2 | 3.7 | [1]_ |
| closed structure, | | | | |
| large water footprint | | | | |
+-------------------------+-------------+--------------------------------+----------------------------------------+-----------+
| Monofacial module, | Singapore | 34.8 | 0.8 | [1]_ |
| closed structure, | | | | |
| large water footprint | | | | |
+-------------------------+-------------+--------------------------------+----------------------------------------+-----------+
| Monofacial module, | Singapore | 18.9 | 8.9 | [1]_ |
| closed stucuture, | | | | |
| medium water footprint | | | | |
+-------------------------+-------------+--------------------------------+----------------------------------------+-----------+
| Monofacial module, | Singapore | 35.3 | 8.9 | [1]_ |
| open strucuture, | | | | |
| free-standing | | | | |
+-------------------------+-------------+--------------------------------+----------------------------------------+-----------+
| Monofacial module, | Norway | 86.5 | 0 | [2]_ |
| in contact with | | | | |
| water | | | | |
+-------------------------+-------------+--------------------------------+----------------------------------------+-----------+
| Monofacial module, | South Italy | 31.9 | 1.5 | [3]_ |
| open structure, | | | | |
| free-standing | | | | |
+-------------------------+-------------+--------------------------------+----------------------------------------+-----------+
| Bifacial module, | South Italy | 35.2 | 1.5 | [3]_ |
| open structure, | | | | |
| free-standing | | | | |
+-------------------------+-------------+--------------------------------+----------------------------------------+-----------+
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References
----------
.. [1] Dörenkämper M., Wahed A., Kumar A., de Jong M., Kroon J., Reindl T.
(2021), 'The cooling effect of floating PV in two different climate zones:
A comparison of field test data from the Netherlands and Singapore'
Solar Energy, vol. 214, pp. 239-247, :doi:`10.1016/j.solener.2020.11.029`.

.. [2] Kjeldstad T., Lindholm D., Marstein E., Selj J. (2021), 'Cooling of
floating photovoltaics and the importance of water temperature', Solar
Energy, vol. 218, pp. 544-551, :doi:`10.1016/j.solener.2021.03.022`.

.. [3] Tina G.M., Scavo F.B., Merlo L., Bizzarri F. (2021), 'Comparative
analysis of monofacial and bifacial photovoltaic modules for floating
power plants', Applied Energy, vol 281, pp. 116084,
:doi:`10.1016/j.apenergy.2020.116084`.
""" # noqa: E501

# %%
# Read example weather data
# ^^^^^^^^^^^^^^^^^^^^^^^^^
# Read weather data from a TMY3 file and calculate the solar position and
# the plane-of-array irradiance.

import pvlib
import matplotlib.pyplot as plt
from pathlib import Path

# Assume a FPV system on a lake with the following specifications
tilt = 30 # degrees
azimuth = 180 # south-facing

# Datafile found in the pvlib distribution
data_file = Path(pvlib.__path__[0]).joinpath('data', '723170TYA.CSV')

tmy, metadata = pvlib.iotools.read_tmy3(
data_file, coerce_year=2002, map_variables=True
)
tmy = tmy.filter(
['ghi', 'dni', 'dni_extra', 'dhi', 'temp_air', 'wind_speed', 'pressure']
) # remaining columns are not needed
tmy = tmy['2002-06-06 00:00':'2002-06-06 23:59'] # select period

solar_position = pvlib.solarposition.get_solarposition(
# TMY timestamp is at end of hour, so shift to center of interval
tmy.index.shift(freq='-30T'),
latitude=metadata['latitude'],
longitude=metadata['longitude'],
altitude=metadata['altitude'],
pressure=tmy['pressure'] * 100, # convert from millibar to Pa
temperature=tmy['temp_air'],
)
solar_position.index = tmy.index # reset index to end of the hour

# Albedo calculation for inland water bodies
albedo = pvlib.albedo.inland_water_dvoracek(
solar_elevation=solar_position['elevation'],
surface_condition='clear_water_no_waves'
)

# Use transposition model to find plane-of-array irradiance
irradiance = pvlib.irradiance.get_total_irradiance(
surface_tilt=tilt,
surface_azimuth=azimuth,
solar_zenith=solar_position['apparent_zenith'],
solar_azimuth=solar_position['azimuth'],
dni=tmy['dni'],
dni_extra=tmy['dni_extra'],
ghi=tmy['ghi'],
dhi=tmy['dhi'],
albedo=albedo,
model='haydavies'
)

# %%
# Calculate and plot cell temperature
# ^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^
# The temperature of the PV cell is calculated for lake-based floating PV
# systems:

# Make a dictionary containing all the sets of coefficients presented in the
# above table.
heat_loss_coeffs = {
'open_structure_small_footprint_tracking_NL': [24.4, 6.5],
'closed_structure_large_footprint_NL': [25.2, 3.7],
'closed_structure_large_footprint_SG': [34.8, 0.8],
'closed_structure_medium_footprint_SG': [18.9, 8.9],
'open_structure_free_standing_SG': [35.3, 8.9],
'in_contact_with_water_NO': [86.5, 0],
'open_strucutre_free_standing_IT': [31.9, 1.5],
'open_strucutre_free_standing_bifacial_IT': [35.2, 1.5],
'default_PVSyst_coeffs_for_land_systems': [29.0, 0]
}

# Plot the cell temperature for each set of the above heat loss coefficients
for coeffs in heat_loss_coeffs:
T_cell = pvlib.temperature.pvsyst_cell(
poa_global=irradiance['poa_global'],
temp_air=tmy['temp_air'],
wind_speed=tmy['wind_speed'],
u_c=heat_loss_coeffs[coeffs][0],
u_v=heat_loss_coeffs[coeffs][1]
)
# Convert Dataframe Indexes to Hour format to make plotting easier
T_cell.index = T_cell.index.strftime("%H")
plt.plot(T_cell, label=coeffs)

plt.xlabel('Hour')
plt.ylabel('PV cell temperature\n$[°C]$')
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plt.ylim(20, 45)
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plt.xlim('06', '20')
plt.grid()
plt.legend(loc='upper left', frameon=False, ncols=2, fontsize='x-small',
bbox_to_anchor=(0, -0.2))
plt.tight_layout()
plt.show()

# %%
# The above figure illustrates the necessity of choosing appropriate heat loss
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# coefficients when using the PVSyst model for calculating the cell temperature
# for floating PV systems. A difference of up to 11.5 °C was obtained when
# using the default PVSyst coefficients and the coefficients when the panels
# are in contact with water.
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