Introduction
As we look ahead to 2025, ACES is taking this opportunity to reflect on climate trends globally, nationally, and locally in the Roaring Fork Watershed. Moving forward, our newsletter will include more regular updates examining how recent local weather events and climate conditions compare to historical trends. Additionally, as we’re doing here, we’ll continue to place these patterns within the broader context of Earth’s climate system—highlighting when our local experience aligns with global trends and when it diverges.
A Note on datasets
There are many historical climate datasets to choose from, and several factors to consider when selecting one. For global and national analyses, we’re using NOAA temperature anomaly data. The global version of this dataset extends back to 1850, while the national dataset begins in 1895.
For state and local analyses, we’re using a combination of the NOAA Monthly U.S. Climate Gridded Dataset, which begins in 1895, and the gridMet dataset, which begins in 1979. Unlike the other datasets, gridMet data is daily, allowing for a more detailed analysis of extreme events. While all of these datasets incorporate station data (e.g., weather stations at airports or SNOTEL stations), we do not explicitly analyze individual stations. Station data is often messy and requires quality control before it can be used in this type of analysis. For example, if a station is relocated to a different elevation or its equipment is changed, it can introduce a warm or cold bias compared to historical data. The datasets we rely on have already been adjusted to account for these discrepancies.