Gulf of Maine Warming Update: Spring 2024

Reports | Jul 2, 2024

Over the past decade, scientists have led a body of research that highlights the rapid pace of warming in the Gulf of Maine. To help keep you informed, we share seasonal and annual updates about conditions in the Gulf of Maine.

Read on for an inside look at what we've learned in our spring 2024 Gulf of Maine warming update.

A title card for the spring 2024 update.
Averaged over the entire season, this table shows that spring SSTs this year were +1.05°F above normal, with weekly SST anomalies ranging from -0.90°F to +3.55°F.
Table 1. Observed weekly average SST, climatological average SST for that week, and SST anomaly (i.e., deviation from the climatological average) in the Gulf of Maine during spring 2024.
Table 2 shows monthly average SST for spring 2024. March SSTs were slightly above the 1991-2020 CRP, with SST anomalies increasing during April and again in May.
Table 2. Monthly ranking, observed average, climatological average, and deviation from the CRP average (i.e., temperature anomaly) for SST at a monthly resolution in the Gulf of Maine during spring 2024.
Figure 1. A ranking of the 15 warmest spring seasons for the Gulf of Maine in the satellite record (1982 – 2023). 2024 was the 11th warmest spring on record.
Figure 1. A ranking of the 15 warmest spring seasons for the Gulf of Maine in the satellite record (1982 – 2023). 2024 was the 11th warmest spring on record.
A figure that shows that the spring rate of warming for the Gulf of Maine (0.56°F per decade) is roughly 2.5x as fast as the spring warming rate globally (0.23°F per decade).
Figure 2. Average annual spring SST anomalies in the Gulf of Maine from 1982 through 2024 (black dots). The orange line indicates the trend for the full timeseries for the Gulf of Maine. The blue line indicates the trend for the full timeseries for the global oceans.
A graph showing that the Gulf of Maine has experienced MHW conditions for 9% of days this spring, beginning at the end of May and extending into the start of summer.
Figure 3. A timeseries of marine heatwave (MHW) conditions in the Gulf of Maine extending from January 1, 2024 through May 31, 2024. Black lines represent the long-term (i.e., 1991 – 2020) average SST, the 10th percentile, and 90th percentile for a given day in the Gulf of Maine; a solid line (red for marine heatwave or blue for a non-event) indicates the observed SST this year; red (above 90th percentile) and blue (below 90th percentile) shading illustrates how far the observed SST is from the climatological average.
A heatmap showing that the relatively cool spring in the Gulf of Maine this year was an extension of cooler fall conditions, which persisted through the 2023-2024 winter, and can be partially attributable to the shift from El Niño to La Niña conditions globally.
Figure 5. Heat map of daily SST anomalies from the beginning of 1982 through May 2024. Not only do more large warm anomalies (darker reds) appear more frequently in recent years, but the frequency, duration, and intensity of marine heatwave events (black lines) in the Gulf of Maine has become more pronounced in the past decade. The re-emergence of cool anomalies in late 2023 / early 2024 is driven, in part, by the transition from El Niño to La Niña conditions, globally.
A map showing that when viewed spatially, almost the entire Gulf of Maine region studied experienced above-average SSTs during spring of 2024.
Figure 5. Map of average SST anomalies for each grid cell in the satellite record for spring 2024. The box outlined by the black dashed line denotes the region of study for the analysis (see Figure 7). Darker red regions indicate warmer anomalies. Black contours have been added at 100m and 200m depths.
This series of maps shows the monthly average SST anomaly for March, April, and May 2024. The region experienced above average temperature anomalies in each season.
Figure 6. This series of maps shows the monthly average SST anomaly for March, April, and May 2024. The box outlined by the black dashed line denotes the region of study for the analysis. Darker red regions indicate warmer anomalies.

Spring 2024 may have felt relatively cool — and, indeed, it was in comparison to the past three years. The main driver of that cooling has been the global transition from El Niño to La Niña conditions. But the long-term trend in warming, both here in the Gulf of Maine and globally, remains undeniable — and will persist.

Dave Reidmiller, Ph.D. Director, Climate Center
This is the staff photo for david reidmiller
Dave Reidmiller, Ph.D. Director, Climate Center
Figure 7. Spatial domain used for Gulf of Maine SST analyses.
Figure 7. Spatial domain used for Gulf of Maine SST analyses. Depth contours are colored at 100 m intervals up to 600 m; deeper blues indicate deeper water depths

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