Last updated: February 14, 2022
Article
2021 Weather in Review: Sagamore Hill National Historic Site
Weather and climate play significant roles in driving both physical and ecological processes. For example, the active processes that shape the North Atlantic coastline are largely the result of meteorological events such as wind-driven waves. For research and long-term ecological monitoring, weather and climate data provide the potential for correlations to be made with observed physical and ecological pattern data.
This article provides a summary of both historic and current (2021) weather data for Sagamore Hill National Historic Site (SAHI), New York (NY). Because tide levels and wind can be significant for coastal parks, the annual water level and wind data are included. Individual weather station data may vary from what is reported here. Data are available from the National Climate Data Center.
Temperature
Overall, 2021 was the 4th warmest year on record with an average temperature of 55.7°F — 3.5 degrees above average (Table 1). 2021 also had the 3rd warmest autumn on record. The warmest month was August with an average of 76.6°F — 3.8 degrees above the monthly average. Seasonally, autumn, summer, and spring fell within “much above normal” temperatures, while winter fell within “above normal” temperatures (Figure 1).
Month (2021) | Average temperature (°F) | Departure from long-term average temperature (°F) |
---|---|---|
January | 34.5 | +3.6 |
February | 33.2 | +1.8 |
March | 43.7 | +4.5 |
April | 52.1 | +3.0 |
May | 60.7 | +1.3 |
June | 72.0 | +3.3 |
July | 75.5 | +1.2 |
August | 76.6 | +3.8 |
September | 70.0 | +3.8 |
October | 62.2 | +6.7 |
November | 45.6 | +0.7 |
December | 42.8 | +7.8 |
Annual | 55.7 | +3.5 |
Precipitation
Overall, 2021 was the 53rd driest year on record with a total of 45.24 inches — only 0.36 inches above the average annual precipitation (Table 2). November had the least precipitation with only 0.86 inches — 2.71 inches below average, while August had the greatest amount in 2021 with 7.35 inches— 3.19 inches above average. Seasonally, spring, autumn, and winter and fell within “below normal” levels, while summer reached “much above normal” levels.
Month (2021) | Total precipitation (in) | Departure from long-term average precipitation (in) |
---|---|---|
January | 2.16 | -1.27 |
February | 4.10 | +0.84 |
March | 3.21 | -0.92 |
April | 2.96 | -0.88 |
May | 4.25 | +0.45 |
June | 2.13 | -1.49 |
July | 6.12 | +2.14 |
August | 7.35 | +3.19 |
September | 6.05 | +2.37 |
October | 4.74 | +1.13 |
November | 0.86 | -2.71 |
December | 1.31 | -2.49 |
Annual | 45.24 | +0.36 |
Temperature and Precipitation Trends (1895–2021)
Temperature and precipitation data are gathered from the U.S. Climate Divisional Database, which stores data from January 1895 to the present, and can be accessed via the National Oceanic and Atmospheric Administration’s (NOAA) National Centers for Environmental Information (NCEI) website (Figure 3). Users can choose different geographic scales (i.e., global, national, statewide), different temporal scales, and display them in various types of graphical formats. Temperature and precipitation data presented in this brief are for Nassau County, NY.
Wind
Wind data (wind speed and direction ) is collected from the NOAA National Water Level Observation Network (NWLON) station 8516945 in Kings Point, NY. Located on the sheltered northwest side of Long Island, this station has records dating back to 1998.
Each direction is divided up into categories called bins that are color coated to represent the frequency of a certain wind speed. The length of the bin represents the number of times wind comes from a given direction as well as the speed of the wind. The longer the length of the bin, the more frequent the given speed was recorded (Figure 4).
Tide Levels
Water level data was also collected from the NOAA NWLON station 8516945 located at Kings Point, NY. The data is graphed to show the difference in the predicted tide level verses what was observed (Figure 5). The offsets in height reflect the effect from storm surge on the normal, astronomically driven tide level.