1.
Please provide your organization’s feedback on the changes being considered to the inputs and assumptions.
CAISO presentation indicates sensitivity of hydro generation modeling inputs (low, average, high hydro years) impacting Loss of Load Expectation (LOLE) studies. CAISO plans to use average hydro year for modeling inputs. With regard to modeling hydro on an average hydro year as well as annual or seasonal only RA showings, CDWR has following comment:
Forecast of pumping load and associated hydro generation that is part of the California Department of Water Resources (CDWR) water delivery system operation is primarily dependent on the forecast of hydrology, water demand, and operational constraints. The California water year hydrologic forecast[1] starts in December and continues monthly with an official declaration of water year hydrologic forecast on May 1st of each water year (e.g. the 2024 water year is 2023 October 1 through 2024 September 30) for the Sacramento Valley and San Joaquin River Valley water year hydrologic classification. SWP operations forecasting mimics the hydrologic forecasting process with monthly updates. Forecast of CDWR pumping load and hydro resources done after May 1st tend to be closer to the actual operation compared to the prior month’s forecasts with a gradual improvement in the forecast each month starting December. However, CDWR must file annual RA plans on October of the prior year that includes demand and hydro supply resources forecasts for the net qualifying capacity(NQC) for the upcoming RA compliance year. Due to uncertainty in hydrology forecast from October prior year and the May 1st next year (RA compliance year) and the following months, there could be significant differences of forecasts between the annual and monthly plan timeframe undermining true reflection of contribution to real time grid reliability both in terms or demand and the supply. As a solution, entities like CDWR with pumping load and hydro generation, monthly update of loads and resources must be allowed as it is done today. Doing so will enable updating demand as well as supply to reflect in the monthly plans and associated RA must offer requirements. Using monthly showings will better reflect the hydrology forecast, water pumping demand, and hydro generation in short-term RA planning, which will enhance the objective of RA.
It is to be noted that:
a) average hydro year (example:2018 used by CAISO) refers to the Below Normal (BN) water year hydrologic classification if the water year classification is based on the California hydrologic forecast.
b) a water year covers the period October 1 through September 30; the water year 2024 starts on October 1, 2023, and ends on September 30, 2024. In contrast, RA compliance year starts on January 1 and ends on December 31st each year. It should be clarified whether hydro capacity monthly NQC values in the modeling correspond to months of the water year type or the RA compliance year months.
c) water year hydrologic classification is done by two regions: Sacramento valley and San Joaquin valley and classification could be different for the two regions for the same year; resources belonging to each area may be associated with a different hydrologic forecast.
d) The California water year hydrologic forecast and water year type classification may impact the capability estimates of any hydro generation (within California) facility. This implies that hydro generation capability updates within a year could be beneficial and applicable to all hydro generating resources for a more realistic availability.
Following are the comments / questions with regard to Slide 14:
a) (Hydro modeling and Weather Year alignment in the stochastic profile)-. If an average hydro year is assumed for short term LOLE studies, how does the weather year alignment take place in terms of timing (e.g., CA water year hydrologic forecast update schedule)? For example, with the official classification of water year type forecast on May 1st, will the stochastic modeling be updated for alignment with the forecasted water year hydrology for that year?
b) Loss of Load and reserve sharing (also in slide 26): Can’t non-spin reserve help avoid Loss of Load as the award to non-spin results in the real time energy (dispatch to generate or drop load)? If it does, then why not include such reserves and resources providing such products in the model in the study (and count them as RA resources)?
[1] Department of Water Resources / California Cooperative Snow Surveys / Sacramento Valley & San Joaquin Valley Water Year Hydrologic Classification: Year types are set by first of month forecasts beginning in December and monthly thereafter. Final determination is based on the May 1st forecast.
https://cdec.water.ca.gov/reportapp/javareports?name=WSIHIST
https://cdec.water.ca.gov/reportapp/javareports?name=WSI (for 2024)
3.
Please provide your organization’s feedback on the capacity accreditation methods and PRM approaches presented today.
For the best option on accreditation among the three (LOLE hours focused, risk hours focused, ELCC based), further analysis may determine which option would be the best for reliability.
PRM (monthly, seasonal, annual): further data analysis on these options may provide some clue.