Gulf of Maine Warming Update: 2023

A Top-Five Hottest Year Despite Relief from Major Storm Systems

Author

Adam Kemberling

Published

February 8, 2024

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

Highlights from the Year

  • With an annual average sea surface temperature (SST) of 52.6°F — more than 1.94°F above normal — the Gulf of Maine experienced its 5th warmest year on record in 2023. This year fell short of the previous warmest year on record — 2021 — 1.49°F, but was record-breaking in a number of regards.

  • The first four months this year average monthly SST was within the top 3 warmest among all years on record. With February, March, and April all the warmest on record.

  • The most extreme temperatures in 2023 occurred in February and March, each setting new records for highest monthly average SST in the Gulf of Maine.

  • The “coolest” monthly average temperature anomalies for 2023 occurred during September, November, and December. Each of last five months this year had SSTs below the top ten warmest.

  • SSTs in 2023 were consistent with the long-term trend of increasingly warm conditions driven primarily by anthropogenic climate change.

2023: SSTs Across the North Atlantic

In a departure from the now-familiar pattern of regionally concentrated warming, much of the attention this year was on large areas in the eastern Atlantic experiencing a large-scale MHW event. This summer scientists sounded the alarm over record setting temperatures for much of the Eastern Atlantic impacting population centers along the European coast and contributing to sweltering temperatures on land.

Beginning in March, the North Atlantic as a whole began experience day-after-day of record warm sea surface temperatures, particularly in the east near Europe. By June and July, the separation between the region’s SSTs and the previous records had widened by over a degree, creating a dramatic and alarming figure that was shared widely on social media. Figure 2 captures how profoundly and consistently hot this year’s temperatures were across the North Atlantic. SST in the North Atlantic set daily record highs for a total of 301 days this year (82%!). Every single day beginning on March 5th has set a new record daily SST values, with margins exceeding 1F. These facts have drawn increased attention, elevated concerns, and a renewed sense of urgency for understanding the causes behind the rapidly changing ocean environment.

Figure 2: Timeseries for each of the three years that hold record daily SSTs for the North Atlantic (2020 = light green, 2022 = blue, 2023 = orange), record setting SSTs shown in bold. The 1991-2020 average daily SST (black) and 10th - 90th percentile range is shown in gray.

2023: SST in the Gulf of Maine

As these broad regional patterns transpired, the Gulf of Maine was experiencing a range of conditions that stood in contrast to recent years and the timing of the North Atlantic’s record temperatures.

What began as one of the warmest years on record for the Gulf of Maine ended on the cooler side, with seasonal conditions not seen in the last decade.

Figure 3: Timeseries for each of the three years that hold record daily SSTs for the North Atlantic (2020 = light green, 2022 = blue, 2023 = orange), record setting SSTs shown in bold. The 1991-2020 average daily SST (black) and 10th - 90th percentile range is shown in gray.

Figure 4: Storm track followed by extratropical storm Lee (orange) as it traversed the Gulf of Maine.

Air-Sea Interactions: Extratropical Storm Lee

Observed SSTs may both influence and be influenced by atmospheric weather patterns. These interactions can act to amplify warming or cooling of surface waters. Sustained periods of low cloud cover and the consequent direct sunlight can rapidly warm the ocean at the surface. Steady winds can act as a fan, advecting heat away from the ocean and cooling the surface. Strong winds and storm systems may also lower SST through mixing, which can bring cooler water from depth closer to the surface.

During September, extratropical storm Lee traversed the Gulf of Maine, which weakened from hurricane strength as it crossed over Georges Bank on September 16 Figure 4. The impacts of this storm on the region’s SSTs can be seen in Figure 3 when temperature fell over 5F over a period of 12 days.

Similar storm crossings have occurred in the recent past, including in 2019 when Hurricane Dorian passed through the Gulf of Maine after working its way up the US East Coast. Both years had some of the fewest autumn heatwave days seen in the past two decades (2019: 0 days, 2023: 6 days).

Comparing Annual SST to Historical Conditions

When we compare the annual average SST in the Gulf of Maine for 2023 (52.6°F) to other years, we can see it narrowly beat out 2012 as the second warmest year on record. When we look at the deviation from the long-term average SST (i.e., the annual SST anomaly), the last decade stands out for its exceptional warmth (Figure 5). 2023 extends a pattern that began in 2010 of sustained above-average temperatures. With the exception of 2019 (ranked 13th), every one of the last ten years remains in the top 10 warmest years on record.

Figure 5: A ranking of the top 10 annual SST values and those years’ respective SST anomalies.

Average Monthly Conditions

Monthly average SSTs (Table 1.) show how variable conditions were throughout the year. For the first third of the year, monthly SSTs were among the top three warmest for those months. May, June, July, & August average SSTs ranked lower, ranging from 4th to 12th warmest. The final four months were each much cooler, ranging from 12th to 19th warmest for those months.

Table 1:

Average monthly sea surface temperatures in the Gulf of Maine

Table 1. Monthly Average Sea Surface Temperatures - 2023
Month Rank (1982-2023) Observed Temperature Climatological Average Temperature Anomaly

January

3

46.5°F (8.1°C)

43.5°F (6.4°C)

3.0°F (1.7°C)

February

1

45.0°F (7.2°C)

40.9°F (5.0°C)

4.1°F (2.3°C)

March

1

43.7°F (6.5°C)

40.1°F (4.5°C)

3.6°F (2.0°C)

April

1

45.2°F (7.4°C)

41.8°F (5.5°C)

3.4°F (1.9°C)

May

6

48.2°F (9.0°C)

46.5°F (8.1°C)

1.6°F (0.9°C)

June

9

54.9°F (12.7°C)

53.5°F (11.9°C)

1.4°F (0.8°C)

July

4

63.6°F (17.5°C)

60.5°F (15.8°C)

3.1°F (1.7°C)

August

12

64.4°F (18.0°C)

63.2°F (17.3°C)

1.2°F (0.7°C)

September

14

61.8°F (16.6°C)

61.2°F (16.2°C)

0.6°F (0.3°C)

October

12

57.7°F (14.3°C)

56.7°F (13.7°C)

1.1°F (0.6°C)

November

16

52.2°F (11.2°C)

51.7°F (11.0°C)

0.5°F (0.3°C)

December

19

47.3°F (8.5°C)

47.4°F (8.6°C)

-0.1°F (-0.1°C)

Data Source: NOAA OISSTv2 Daily Sea Surface Temperature Data.
Climatological Reference Period: 1991-2020.

Daily SSTs in the Gulf of Maine

The annual cycle of SST in the Gulf of Maine exhibits a pattern common to regions in the Northern Hemisphere, with the lowest temperatures observed in March and the highest values observed in August (Figure 6). Daily SST anomalies in 2023 never fell below +-1.79 °F compared to the long-term (1991-2020) average and reached as high as high as 5 °F above the long-term average.

The largest temperature anomalies were observed during November, which also turned out to be the warmest November on record (as highlighted in our Fall 2022 update). Figure 6 also illustrates that, in 2023, 135 days experienced SST anomalies that exceeded the threshold for being considered marine heatwaves, or MHW (more on MHWs below, including Figure 10)

Figure 6: A timeseries of daily SSTs (January 1 through December 31, 2023) with an indication of marine heatwave (MHW) conditions in the Gulf of Maine. Black lines represent the long-term (i.e., 1991 – 2020) average SST, the 10th percentile (i.e., cold spell threshold), and 90th percentile (i.e., heatwave threshold). A solid line indicates the observed SST for each day; red and blue shading illustrates whether each day is considered part of a MHW event.

SST Anomalis & MHW Events

A marine heatwave (MHW) is defined as a period when there are five or more consecutive days when the observed SST is greater than the 90th percentile of the long-term average for that day. Gaps of 2 days or less in this threshold do not constitute a break in the MHW event. Figure 6 illustrates that the Gulf of Maine met the criteria for experiencing a MHW for 135 days in 2023 (or 97% of the year). Superimposing MHW status (black line) over the full timeseries of daily SST anomalies (blue/white/red shading) (Figure 6) reveals that the frequency, duration, and intensity of MHWs has increased in the past decade.

Figure 7: A timeseries of marine heatwave (MHW) conditions in the Gulf of Maine extending from January 1, 2023 through December 31, 2023. The black line represents the long-term (i.e., 1991 – 2020) average SST. The 10th to 90th percentile range is shaded in gray. The heavy line (red for marine heatwave or blue for a non-event) indicates the observed SST this year.

Record Setting Daily Sea Surface Temperatures

Daily SST values in 2023 were some of the highest ever recorded in the Gulf of Maine. Record high SSTs were set for more than half of all days during the months of February, March, & April. February saw the most new records, with 86% of days setting new daily record highs.

Figure 8: Percentage of days during each month in 2023 during which SSTs set record-high temperatures in the Gulf of Maine (e.g. 86% — 24 days — of February were new record-setting high temperatures).

Decline of Below Average SST Temperature Days

As SST in the Gulf of Maine continues to rise, the fraction of days when the region experiences below-average temperatures is expected to continue to fall. In a world without human-caused climate change, we would expect, positive (warm) and negative (cool) SST anomalies to more or less balance out over the span of several years, as various patterns of natural climate variability alternate having a dominant influence on Earth’s climate (e.g., La Niña vs El Niño). What is being observed in the Gulf of Maine (and elsewhere around the world), however, is a loss of that balance: larger fractions of recent years are experiencing above average temperatures and cold spells are becoming vanishingly rare.

During 2023 the Gulf of Maine experienced SSTs below the long-term average for a total of 48 days. A period of less than 2 months, and with no days experiencing temperatures that would qualify as marine cold-spells, the cool-water equivalent of a MHW. These events have become rare, with just 5 days of cold spell conditions in the last 20 years.

Figure 9: The total number of days below mean climatological average SST (dark blue) and days with SSTs below the 10th percentile (light blue) from the 1991-2020 climatological baseline.

Gulf of Maine SSTs Out of Balance

The complete picture of above and below average conditions for the Gulf of Maine reveals a region out of balance. Since 2010 the Gulf of Maine has experienced a disproportionate number of anomalously hot SSTs and experienced many prolonged MHW events.

A figure displays the temperatures for each day of year as a colored stripe, organized with a row for each day such that the day of year aligns vertically. The lower two-thirds has a roughly equal balance between colors for warm (red) and cold (blue) temperature anomalies. The top third of the image is almost completely red as temperature anomalies rarely fall below the long-term average. Black dots are overlaid onto days that meet the criteria for a heatwave, they are rare in the lower section and common in the red section.

Figure 10: Heat map of daily SST anomalies from the beginning of 1982 through the end of 2023. Not only do more large warm anomalies (darker reds) appear more frequently in recent years, but the frequency and duration of marine heatwave events (black lines) in the Gulf of Maine has become more pronounced in the past decade.

Annual SST Anomaly Map

In addition to the sub-annual (or temporal) variation, there can also be significant spatial variability in annually-averaged SST patterns (Figure 12).

This year the impacts of large-scale variability in major oceanic currents, such as the relative influence of the Gulf Stream versus the Labrador Current was quite apparent. With large pockets of above and below average SST anomalies present along the turbulent path of the Gulf Stream to the South of our study area.

Figure 12: Map of annual average sea surface temperature anomalies in 2023. The box outlined by the black dashed line denotes the region of study for the analysis presented throughout this report.

Quarterly Average SST Maps

Looking at these spatial patterns across the annual quarters of 2023 (Figure 13) shows not only the large spatial variability in SST conditions, but also the significant variation in those patterns over the course of the year.

Figure 13: Four-panel maps displaying the quarterly average SST anomalies in 2023.

Comparison to Global Temperatures

It was not just the Gulf of Maine that experienced exceptional warmth in 2023. Globally, 2023 was the warmest year for both sea surface temperatures and combined land & ocean temperatures.

Figure 15 shows annual average SST anomalies for oceans all over the world in 2023. From this view we can see how much of the Southern Ocean and expanses of the southeastern Pacific were anomalously warm (a general feature of El Niño conditions). Closer to home here in the United States, we see both unusually high and unusually low SSTs along the Gulf Stream’s path as it extends East away from Cape Hatteras.

Figure 14: Map of annual average sea surface temperature for the world’s oceans in 2023.

Figure 15: Map of annual average sea surface temperature anomalies for the world’s oceans in 2023.

Warming Rates of the Global Ocean

Percentile Warming Ranks

Figure 16: ?(caption)

The Importance of the Gulf of Maine Region

For analyses like these that characterize environmental conditions for a particular area—in this case, the Gulf of Maine—it is important to be clear about the spatial extent that defines the region of study; different domain boundaries could produce different results. The spatial area we use to define the “Gulf of Maine” is displayed in Figure 17, and has remained consistent throughout our seasonal and annual warming updates.

An overhead view of the Gulf of Maine region. Landmasses and political boundaries for the United States and Canada are displayed. A blue dotted line outlining a box with a transparent blue fill is shown to demark where satellite data for the analysis has been used.

Figure 17: Spatial domain used for Gulf of Maine SST analyses. Dashed line denotes the region of study for this analysis. Depth contours are colored at 100m intervals to a maximum of 600m, deeper blues indicate deeper water depths.

A Note on Data Sources

The figures in this report are created using remotely-sensed satellite data as part of publicly funded research efforts. Satellite SST data was obtained from NOAA’s National Center for Environmental Information (NCEI), with all maps and figures displaying NOAA’s Optimum Interpolation Sea Surface Temperature Data.

  • NOAA High Resolution SST data provided by the NOAA/OAR/ESRL PSL, Boulder, Colorado, USA, from their Web site at https://psl.noaa.gov/data/gridded/data.noaa.oisst.v2.highres.html.

Recommended Citation:

Gulf of Maine Research Institute. 2023. Gulf of Maine Warming Update: 2023. https://gmri.org/stories/warming-22


 

A work by Adam A. Kemberling

Akemberling@gmri.org