Article

Climate and Water Monitoring at Fort Union National Monument: Water Year 2024

Brown mud ruin walls in a valley of snow covered grasses with snow covered mountains behind them.
Fort Union National Monument, New Mexico

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Overview

Together, climate and hydrology shape ecosystems and the services they provide, particularly in arid and semi-arid ecosystems and across the Southern Plains (Woodhouse and Overpeck 1998). Understanding changes in climate, groundwater, and surface water is key to assessing the condition of park natural resources—and often, cultural resources.

At Fort Union National Monument (Figure 1), Southern Plains Inventory and Monitoring Network scientists study how ecosystems may be changing by taking measurements of key resources, or “vital signs,” year after year—much as a doctor keeps track of a patient’s vital signs. This long-term ecological monitoring provides early warning of potential problems, allowing managers to mitigate them before they become worse. At Fort Union National Monument, we monitor climate and groundwater, among other vital signs.

Groundwater conditions are closely related to climate conditions. Because they are better understood together, we report on climate in conjunction with water resources. Reporting is by water year (WY), which begins in October of the previous calendar year and goes through September of the water year (e.g., WY2024 runs from October 2023 through September 2024). This web report presents the climate and groundwater monitoring results for Fort Union National Monument in WY2024.

Reference: Woodhouse, C. A., and J. T. Overpeck. 1998. 2000 years of drought variability in the central United States. Bulletin of the American Meteorological Society 79(12): 2693–2714. https://doi.org/10.1175/1520-0477(1998)079%3C2693:YODVIT%3E2.0.CO;2

Map of a groundwater well in the southern end of the main park unit
Figure 1. Monitored groundwater well at Fort Union National Monument. Green shaded areas outlined by solid dark green line represent park boundaries.

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Climate and Weather

There is often confusion over the terms “weather” and “climate.” In short, weather describes instantaneous meteorological conditions (e.g., it’s currently raining or snowing, it’s a hot or frigid day), and climate reflects patterns of weather at a given place over longer periods of time (seasons to years). Climate is the primary driver of ecological processes on earth. Climate and weather information provide context for understanding the status or condition of other park resources.

Methods

The closest weather station to Fort Union National Monument is 19 miles (31 km) away. As a substitute, climate analyses in this report use current year and 30-year averages (1991–2020) of gridded surface meteorological (GRIDMET) data from the location of the Fort Union National Monument Visitor Center.

GRIDMET is a spatial climate dataset at a 4-kilometer resolution that is interpolated using weather station data, topography, and other observational and modeled land surface data. Temperature and precipitation estimated from GRIDMET may vary from actual weather at a particular location, depending on the availability of weather station data and the difference in elevation between the location of interest and that assigned to a grid cell. Data from the weather station 19 miles from the park and GRIDMET are available through Climate Analyzer.

Grassland plants glowing with the setting sunlight .
Fort Union National Monument, New Mexico

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Results

Precipitation

Annual precipitation at Fort Union National Monument in WY2024 was 18.66″ (47.4 cm), 1.28″ (3.3 cm) more than the 1991–2020 annual average. Precipitation totals in December, March, and June were substantially wetter than the 1991–2020 averages by up to 1.87″ (4.7 cm; Figure 2). November, April, and September were substantially drier than the averages, by up to 0.88″ (2.2 cm). Monthly precipitation during the other six months was similar to the long-term averages.

Air Temperature

The mean annual maximum temperature at Fort Union National Monument in WY2024 was 65.8°F (18.8°C), which is exactly the same as the 1991–2020 average. The mean annual minimum temperature in WY2024 was 35.1°F (1.7°C), 2.1°F (1.1°C) above the 1991–2020 average. Mean monthly maximum and minimum temperatures for WY2024 differed by as much as 5.4°F (3.0°C; see June as an example). However, mean monthly maximum temperatures were within 2.0°F (1.1°C) of the 1991–2020 monthly averages during most of the year (Figure 2). Mean monthly minimum temperatures were above or similar to average the entire year.

Climogram showing overall maximum temperatures for WY2024 were similar to those for 1991–2020, and minimum air temperatures in WY2024 were slightly higher. Precipitation totals in WY2024 were variable month to month compared to those for 1991–2020.
Figure 2. Climogram showing monthly precipitation and mean maximum and minimum air temperatures in water year (WY) 2024 and the 1991–2020 averages at Fort Union National Monument. Data source: GRIDMET via climateanalyzer.org.

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Drought

Reconnaissance drought index (Tsakiris and Vangelis 2005) provides a measure of drought severity and extent relative to the long-term climate. It is based on the ratio of average precipitation to average potential evapotranspiration (the amount of water loss that would occur from evaporation and plant transpiration if the water supply was unlimited) over short periods of time (seasons to years). The reconnaissance drought index for Fort Union National Monument indicates that WY2024 was wetter than the 1991–2024 average from the perspective of both precipitation and potential evapotranspiration, after a four-year period of drier than average conditions (Figure 3).

Reference: Tsakiris G., and H. Vangelis. 2005. Establishing a drought index incorporating evapotranspiration. European Water 9: 3–11.

Bar graph showing conditions in WY2024 were wetter than average.
Figure 3. Reconnaissance drought index for Fort Union National Monument, water years (WY) 1991–2024. Drought index calculations are relative to the time period selected (1990–2024). Choosing a different set of start/end points may produce different results. Data source: GRIDMET via climateanalyzer.org.

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Early morning frost on the plains surrounding Fort Union.
Early morning frost on the plains surrounding Fort Union.

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Groundwater

Groundwater is one of the most critical natural resources of the American Southwest and Southern Plains. It provides drinking water, irrigates crops, and sustains rivers, streams, and springs throughout the region.

Methods

At Fort Union National Monument, groundwater is monitored using one well (WL-0257; Figure 1). The New Mexico Bureau of Geology and Mineral Resources began monitoring the well in 2022. The data are available at the Healy Collaborative Groundwater Monitoring Network.

Results

Groundwater level was measured once in WY2024 at 93.15 feet below ground surface (ft bgs; 28.39 m bgs) on 10 May 2024 (Table 1 and Figure 4). This measurement is the highest of the four-year record and may represent a recovery from the previous two years. Additional data will be needed to better understand normal groundwater fluctuations at this well.

Line graph of four measurements over four years showing no trend in depth to water in the well.
Figure 4. Depth to water in feet below ground surface (ft bgs) in the monitored groundwater well at Fort Union National Monument, water years (WY) 2021–2024.

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Report Citation

Authors: Kara Raymond, Andy Ray

Raymond, K., and A. Ray. 2025. Climate and Water Monitoring at Fort Union National Monument: Water Year 2024. Southern Plains Network, National Park Service, Pecos, New Mexico.

Fort Union National Monument

Last updated: August 26, 2025