The California Current Marine Heatwave Tracker - Blobtracker

What is a marine heatwave?

Marine heatwaves, or MHWs, occur when ocean temperatures are much warmer than usual for an extended period of time; they are specifically defined by the difference between the current temperature and the expected temperature for a specific location and time of year [1]. MHWs are a growing field of study worldwide because of their effects on ecosystem structure, biodiversity, and regional economies.

In 2014 a large MHW was identified as it began dominating the northeast Pacific Ocean. Eventually known as “The Blob” [2] (Fig. 3A.), this basin-scale MHW was unique in the history of monitoring in the California Current, and persisted until mid-2016. Researchers documented many ecological effects associated with “The Blob”, including unprecedented harmful algal blooms, shifting distributions of marine life, and changes in the marine food web [3].

Large marine heatwaves have occurred each of the last five years (2019 - 2023), all typically beginning during the spring in the far offshore region of the open North Pacific, impacting the US west coast during the fall, and finally terminating during late winter. Of the last five years, four of these were the largest heatwaves on record for the eastern North Pacific since monitoring began in 1982 (calculated only within the analyzed region shown in Fig. 2). However, note some of these heatwaves were likely larger as they extended beyond the borders of this prescribed region at various times. Animations of recent years' heatwaves can be found here..

To further investigate past MHW events, access this table of detailed information (i.e., size, duration, distance from shore) or an archive of past yearly animations.

What are the latest conditions?

(last updated 3 December, 2024)

We continue to track a large (~ 3 million km^2 in area currently) marine heatwave (MHW), denoted as NEP24A (Fig. 1 and 2). This MHW began in late April (~April 28th), slowly grew to approximately 3.5 million km^2 over the summer, decreased slightly in size during late July, and then expanded to its maximum size during August (~6 million km^2 on Sept 3rd), occupying >50% of the west coast Exclusive Economic Zone (EEZ) during late August (Figure 4b; the red shading on the bars indicates > 50% coverage). NEP24A was the 6th largest by area and 7th longest by duration since satellite monitoring began in 1982. This heatwave emerged with the same timing from a similar region far offshore as MHWs have in the past 5 years, and so far this year it has followed the same pattern as previous heatwave events. During October and November, heatwave conditions decreased in the nearshore within the EEZ, while the main body of the heatwave has remained further offshore and is now located in the more southern part of the analyzed region (Fig 1 and 2).   

The current heatwave forecast (https://psl.noaa.gov/marine-heatwaves/) suggests NEP24A will continue to decline in size and strength over the fall in nearshore regions, following the spatiotemporal pattern described above. The El Niño forecast suggests that a weak La Niña is likely to emerge in October-December 2024 and persist through January-March 2025 (see https://www.cpc.ncep.noaa.gov/products/analysis_monitoring/enso_advisory/ensodisc.shtml). We will continue to monitor the area, duration, and coastal proximity of surface water temperatures for these features in the northeast Pacific and communicate with other researchers and policy-makers to understand the array of possible West Coast impacts.

Animations and images of past years' developing heatwaves can be found here: NEP2023A animation; NEP22A animation; previous archived animations.

View new and ongoing analyses highlighting regional conditions associated with individual west coast National Marine Sanctuaries and states (Washington, Oregon, and northern, central, and southern California).

What is the MHW Tracker (aka "Blobtracker")?

Developed by oceanographers from NOAA Fisheries’ Southwest Fisheries Science Center as an experimental tool for natural resource managers, the California Current MHW Tracker (aka “Blobtracker”) is a program designed to describe and thereby provide historical context for current and past large marine heatwaves.  It also produces a range of indices that could help forecast or predict future MHWs expected to impact our coast.

Because “The Blob” dramatically affected natural resources, including economically valuable fisheries, predictive forecasts will help natural resource managers, businesses, and coastal communities anticipate changes and mitigate possible damages in the future.

The California Current MHW Tracker automatically analyzes sea surface temperature anomalies (SSTa) from 1982- present, with a particular focus on detecting the presence of significant ”Blob-Class” events. Sea surface temperature (SST) data were obtained from a variety of different platforms (satellites, ships, buoys) on a regular global grid at a resolution of 1/4°, as provided by NOAA’s OISST program.

Here, we define “Blob-Class” MHWs based on their strength (>1.29 times the standard deviation of the SSTa field; e.g., the top 90% of the data), along with their areal extent (area > 400,000 km², which includes the top 20% of all heatwaves recorded in this region since 1982). The “Blobtracker” program groups all contiguous pixels satisfying the strength threshold, and then tracks those contiguous regions over time, as long as they continue to satisfy the area threshold and spatially overlap at least part of a similar feature from the day before.  This allows the tracking and classification of these large marine heatwaves as they evolve and move around the north Pacific, similar to how one would track large storms or hurricanes.  We have adopted a naming convention for these tracked heatwaves of giving them a number based on the year of their first crossing the area threshold, and a letter corresponding to the order in which they arise each year (e.g. the second “Blob-Class” heatwave that arises in 2010, would be called NEP10b, with the NEP standing for Northeast Pacific).  Besides tracking these large “Blob-Class” features, we also provide indices related to how much of the EEZ (Exclusive economic zone) of the US west coast is in heatwave status, by calculating the % total area within the EEZ exceeding the strength threshold, regardless of the area-tracking threshold (Fig. 4).

What controls the presence of heatwaves near the coastline?

For fisheries management purposes, the most important aspect of these heatwaves are whether they come into close contact with our coasts and within the EEZ, as these are the regions where the majority of our fisheries resources are based.  Although local forces are important, the dominant feature which controls coastal water temperatures in the California Current system (CCS) is alongshore wind patterns. Because of the orientation of the US west coast coastline (predominantly N-S) and the general flow of the CCS (from north to south along the coast), and the effects of coriolis, our coast is heavily impacted by a process known as upwelling. Essentially, when wind blows from north towards the south along this coast, it causes an “upwelling” of deeper, colder, nutrient rich waters to rise to the surface, displacing warmer surface waters offshore. Vice versa, when winds are weak, or blow from south to north, this may shut off (termed upwelling “relaxation”), or even reverse upwelling (termed “downwelling”), which allows surface waters to warm, and/or offshore waters to advect towards the coast.

Therefore, our working hypothesis is that much of the timing and occurrence of large marine heatwaves within the US west coast EEZ is related to changes in the winds driving upwelling. When upwelling winds weaken or reverse, coastal waters tend to warm. Further, when there are already large marine heatwaves in the offshore region, changes in wind direction and strength can lead to those features advecting into, or becoming contiguous with, warmed coastal waters during these upwelling “relaxation” or “downwelling” events if those events last for a significant period of time. Because of the presumed importance of these basin-scale winds driving upwelling patterns, which are in turn driven by basin-scale atmospheric pressure patterns (further described here), we have begun to closely monitor the wind and pressure patterns across this region, along with SSTa (Fig. 1).  

Did marine heatwaves break any records last year?

2023 saw some of the warmest temperatures on record, both on land and at sea. Within the California Current Exclusive Economic Zone (EEZ), we analyzed sea surface temperatures using satellite-based data extending back to 1982 to look for times and locations when new records were set during 2023. We define a “record breaker” as any location where the temperature on a specific day is higher than the previously recorded temperature at that location for that specific day of the year. We found a significant number of times and locations when daily sea surface temperature records were broken during 2023 (Fig. 6), an overwhelming majority of which occurred in the farther offshore regions (>100km from the coast) within the EEZ, rather than the nearshore zone. To the north, most of these record-breaking temperatures occurred during the summer coincident with the intrusion of the large marine heatwave, and included some days that set absolute all-time records for this location on any date since 1982 (Fig. 7). Within the central region comprising offshore regions of northern CA and OR, most temperature records also coincided with the summer heatwave, but some additional records were broken during the late fall/early winter as El Niño conditions arose (Fig. 8). To the south, most records were broken during the late fall/early winter, coincident with the onset of the current El Niño (Fig. 9). Note that in most cases, previous temperature records were set either during the 1997/1998 El Niño or the unprecedented 2014/2015 marine heatwave, known as “The Blob”. 

Project leads

Andrew Leising and Lynn DeWitt (SWFSC), Greg Williams (NWFSC)

References

[1] Hobday, A. J. et al. (2016), A hierarchical approach to defining marine heatwaves, Prog. Ocean., 141, pp. 227-238, 10.1016/j.pocean.2015.12.014

[2] Bond, N. A., Cronin, M. F., Freeland, H., & Mantua, N. (2015). Causes and impacts of the 2014 warm anomaly in the NE Pacific. Geophysical Research Letters, 42, 3414–3420. https://doi.org/10.1002/ 2015GL063306

[3] Cavole LM, Demko AM, Diner RE, Giddings A, Koester I, et al. (2016). Biological impacts of the 2013–2015 warm-water anomaly in the northeast Pacific: winners, losers, and the future. Oceanography 29(2):273–85