Forecasting Building Energy Demands for New York City With a Coupled Weather-Building Energy Model

Abstract

Major metropolitan centers experience challenges during management of peak electrical loads, typically occurring during extreme summer events. These peak loads expose the reliability of the electrical grid and customers may incur in additional charges for peak load management in regulated demand-response markets. This opens the need for the development of analytical tools that can inform building managers and utilities about near future conditions so they are better able to avoid peak demand charges, reducing building operational costs. In this article, we report on a tool and methodology to forecast peak loads at the City Scale using New York City (NYC) as a test case. The city of New York experiences peak electric demand loads that reach up to 11 GW during the summertime, and are projected to increase to over 12 GW by 2025, as reported by the New York Independent System Operator (NYISO). The forecast is based on the Weather Research and Forecast model version 3.5, coupled with a building environment parameterization and building energy model. Urban morphology parameters are assimilated from the New York Primary Land Use Tax Lot Output (PLUTO), while the weather component of the model is initialized daily from the North American Mesoscale (NAM) model. A city-scale analysis is centered in the summer months of June-July 2015 which included an extreme heat event (i.e. heat wave). The 24-hr city-scale weather and energy forecasts show good agreement with the archived data from both weather stations records and energy records by NYISO.

Thermal Structure of a Coastal–Urban Boundary Layer

“…While we present the mean thermal characteristics of the coastal-urban environment here, additional work is necessary to study the turbulent transport of heat, momentum and moisture within the coastal-urban boundary layer. Current numerical weather prediction models used in the study of the urban boundary layer (e.g., Leroyer et al 2014;Gutiérrez et al 2015b;Ortiz et al 2016;Ramamurthy et al 2017b) lack a realistic representation of urban-coastal interactions, since boundary-layer parametrizations are unable to reproduce the thermal internal boundary layers observed. More effort and sustained observations are necessary to improve the predictability of the thermal conditions in the coastal-urban environment.…”