2.1.1. Data and Pre-Processing
The main dataset used in this research is the hourly supply/demand breakdown for the Kyushu region in Japan from April 2016 to September 2019 from Kyuden in 3-month files [
23] and from the Institute for Sustainable Energy Policies (ISEP) in yearly datasets [
11]. The data contain time and date stamps, demand and all the supplies for each hour, all in MWh.
Figure 3 shows monthly average values of the stagnant demand, decreasing thermal supply, increasing nuclear and solar supply, and rapidly increasing curtailment starting from October 2018 in addition to the overall trends. The curtailment occurs in the off-peak seasons, autumn and spring, of demand when nuclear had reached a critical level. The increasing nuclear energy has a clear correlation to curtailment because as it increased, thermal energy decreases. Therefore, there is less flexibility in the energy supply allowing for potentially higher curtailment on days with excess VRE.
Figure 4 shows the hourly variation in the supply and curtailment of the day with the highest curtailment, 7 April 2019, and is key to understanding the behaviour of all supplies when curtailment occurs. Before 5 am, there was no curtailment, and the demand was mostly met with nuclear and thermal energy. There was a constant value of grid interconnection energy being sent to the neighbouring Chugoku region, as well as a small amount of positive pumped storage energy, which indicates that the pumped storage was releasing energy at that time.
Regarding the demand on 7 April 2019, it was a Sunday in spring, and therefore, the demand was quite low. Japan suffers from extreme heat and cold in the summer and winter, respectively, implying that electricity demand peaks at those times, with the troughs being in the spring and autumn.
At 6 am, solar generation began and ramped up quite quickly to its maximum at 12:00. This ramp-up was one of the largest causes of curtailment, as the other supplies could ramp down quickly enough to maintain the balance. As soon as solar generation starts, thermal generation is reduced because the thermal energy reduction is the main form of balancing the supply and demand. However, the thermal generation cannot decrease to zero. It has a minimum amount that it cannot go below. It also has a maximum hourly ramp-down rate that cannot be exceeded.
Table 2 summarizes the monthly solar curtailment between September 2018 and September 2019, and its estimated cost. The curtailment during this period was 2.7%, which is quite low compared to that of other countries. This is further reinforced by the monthly curtailment, where in October 2018, curtailment is only 1.3%. However, from February 2019 to April 2019, the monthly curtailment increased from 0.4% to 6.8% and then 12.1% in April. The curtailment was set to continue in May. The total value of all the curtailments was approx. ¥9.6 billion, with 98% of that coming from solar curtailment. This approximate curtailment cost was calculated using the average FIT tariff for 2012–2015 multiplied by the curtailed energy [
7].
2.1.2. Categorisation of Supplies
Figure 5 shows the energy generation sources in Kyushu for 2018 compared to the nationwide generation. Kyushu generated significantly more electricity from nuclear than the nation as a whole. Only three regions restarted nuclear energy generation in Japan post-2011, with Kansai and Kyushu having the highest energy generation. This is extremely significant to curtailment, as nuclear energy is “non-controllable” and “constant”, and it accounts for 21% of the total energy supplied in Kyushu in 2018. Along with this, solar generation was much higher as well. These are the two main factors affecting curtailment. Furthermore, Kyushu’s thermal generation was much lower than that nationwide, as the high nuclear generation required thermal to decrease; while this is good for the environment, it reduces one of the largest tools to mitigate curtailments. Geothermal in Kyushu was higher than that nationwide but only accounts for 1% of generation, whereas biomass was similar to that nationwide at 1%, again a minimal supply type. Hydro was lower than that nationwide, at 5% in Kyushu. The wind capacity was also similar that nationwide, at 1%.
The hourly sum of the supplies should always equal the demand as described in Equation (1). This condition must be true for each hour and is checked in Step 1 of the methodology:
To forecast the curtailment, each component of Equation (2) must be calculated for each hour. To facilitate forecasting, these power generation types is categorised based on their observed behaviour.
Table 3 depicts the result of classification of power generation types into “controllable” and “non-controllable” with other characteristics such as seasonality, trend, and variability.
Figure 6 depicts the ramp rates, as defined in Equation (3) [
24], of the supplies and demand from 05:00 to 19:00 on 7 April 2019, showing how each type reacted to increasing solar power, thus reinforcing the controllable and non-controllable classification.
where P(t) is the VRE power at the target hour and D is the time duration for which the ramp rate is determined (in this case, 1 h intervals based on the input data).
The main cause of curtailment on this day was solar power, which increased dramatically in the morning, reaching a peak ramp-up rate between 08:00–09:00. Then, it continued to increase at a lower ramp rate up to 12:00, when it started to ramp down. As solar ramped up, the other supply types had to be adjusted to maintain the supply/demand balance, which was what happened initially. However, some types, such as geothermal, biomass, hydro, wind, and nuclear, were not adjusted as the solar ramped up, and they remained mostly constant. These supplies are classified as “non-controllable”, as mentioned earlier, because Kyuden has little to no influence over these supplies. This includes solar, as they cannot control its ramp rate. Demand is also classified as “non-controllable”.
As time progressed, thermal continues ramping down, but it was limited to a maximum ramp down rate of −578 MW/h. The thermal supply presumably approached its minimum generation value at 09:00, and therefore, its ramp rate decreased and eventually approached 0. As this happened, the ramp-up rate of both pumped storage and grid interconnection increased. Grid interconnection, like pumped storage, had a positive and a negative value when it sent more energy to the neighbouring Chugoku region, which was ramping up. However, the large ramp-up of solar power was unable to be matched by the adjustments of the controllable supplies, and therefore, curtailment started ramping up at 07:00, reaching a peak of 685 MW/h between 08:00 and 09:00, as thermal started ramping down.
As the solar ramp-up rate decreased, curtailment continued as peak solar generation occurred at 12:00, and the ramp rate of pumped storage went negative, indicating that the charging rate was reduced, perhaps due to the maximum capacity being reached. Then, the solar ramp rate went negative, indicating that solar was ramping down. In the late afternoon, the ramp-down rate of solar curtailment was reduced to zero; therefore, curtailment stopped at 16:00, at which point thermal started to ramp up, and the balance was maintained as the solar ramp rate was also reduced. Pumped storage had a high ramp down rate between 16:00 and 18:00, as its charging rate decreased to almost zero.
These classifications can be applied to the main supply/demand formula, as defined in Equations (4)–(6):