Mercator Ocean International (MOi) oceanographers examine marine heatwaves across the global ocean. They analyse a variety of datasets from observations (satellite sea surface temperature maps) to numerical model analyses (assimilating satellite and in situ observations) and derive marine heatwave forecasts for a 9 day period.[1]
Forecasts for October 19th
Europe Zone
For the 19th of October, Mercator Ocean International forecasts that the situation remains stable in the Baltic sea and in the Mediterranean Sea, with some moderate and locally severe marine heatwaves in the eastern part of the Mediterranean basin.
Global Ocean
Atlantic Ocean
North Atlantic Ocean – MOI forecasts that marine heatwaves will almost disappear, and only a few small, moderate-category marine heatwaves will persist compared to the 8th of October.
North Tropical Atlantic Ocean – In the tropical North Atlantic, the marine heatwave remained stable in extent, but diminished in intensity, with less surface area in severe categories. In the Gulf of Mexico, the marine heatwave disappears completely.
South Tropical Atlantic Ocean – In the tropical North Atlantic, the marine heatwave remained stable in extent, but diminished in intensity, with less surface area in severe categories. In the Gulf of Mexico, the marine heatwave disappears completely.
Southern Ocean
The marine heat wave in the Southern Ocean, off the South African coast (between 5°W and 90°E) remains stable, with moderate and strong categories.
Pacific Ocean
Tropical Pacific Ocean – In the Tropical Pacific, a strong and locally severe marine heatwave is forming off Central America. The marine heatwave to the west of the basin to the north of Papua New Guinea remains stable overall, with moderate and strong categories.
North Pacific Ocean – In the North Pacific, the marine heatwave in the center of the basin, at around 180°W, is decreasing in extent but remains stable in intensity, with moderate and strong categories. The marine heatwave off the North American coast and around 150°W, is decreasing in intensity, with less surface area in the strong category. Marine heatwaves in the Sea of Japan, China Sea and Yellow Sea remain stable overall, with moderate and strong categories.
South-East Asian Seas –In the Southeast Asian seas, the marine heat wave remains stable overall, with moderate and strong categories.
South Pacific, to the east of New-Zealand –In the South Pacific, to the south of the basin at around 150°W, the marine heat wave diminishes in area until it almost disappears.
Indian Ocean
In the Indian Ocean, Mercator Ocean forecasts that the marine heatwave decreases in extent across the basin, but remains stable in intensity, with moderate and strong categories. With the exception of north-western Australia, where the marine heatwave changes from strong to moderate.
Weekly temperature anomalies
Atlantic Ocean | North 0°C to 2°C | North Tropical 0.5°C to 1.5°C | South Tropical 0°C to 3°C | |
Southern Ocean | -1°C to 3°C | |||
Pacific Ocean | North -1°C to 3°C | Tropical -1°C to 1°C | South 0°C to 1°C | South-East Asian Seas 0.5°C to 1.5°C |
Indian Ocean | 0.5°C to 2°C |
Consult our Daily Global Physical Bulletin for a 9-day forecast here.
What are marine heatwaves?
Marine heatwaves (MHW) are extreme rises in ocean temperature for an extended period of time. They can occur at different locations in the ocean, and their magnitude and frequency have increased over the last couple of decades, with harmful impacts on ecosystems, and human activities. According to the latest report released by the Intergovernmental Panel on Climate Change (IPCC AR6 SYR), it is found with high confidence that in the near-term at 1.5°C global warming, the increasing frequency of marine heatwaves will increase risks of biodiversity loss in the oceans, including from mass mortality events.[2]
How are marine heatwaves calculated?
A marine heatwave is an episode during which the ocean temperature is abnormally warm for at least 5 consecutive days.
Figure adapted from Hobday et al. (2018)
For any location in the ocean, the normal temperatures are defined for every day of the year using a climatological period (here 1993–2016). A heatwave is identified when the measured daily temperature is within the top 10% of the highest recorded values for that day (i.e., above the 90th percentile, see diagram), and with this condition persisting for at least five consecutive days.
The intensity of the heatwave on any given day is measured as the number of degrees above the climatological average (represented by the bold black line) indicated by the blue arrow. We can either calculate the cumulative intensity over the entire heatwave or record the maximum intensity.
Heatwaves are classified based on their intensity level. To do this, the intensity is compared to the difference between the climatological value and the 90th percentile value. A mhw intensity between 1 and 2 times this difference corresponds to a heatwave of moderate category; between 2 and 3 times, to a strong category; between 3 and 4 times, to a severe category; and a difference greater than 4 times corresponds to an extreme category.
[1] Analysis of datasets: SST OSTIA (Copernicus Marine Service), OISST (NOAA), GLO12 (Copernicus Marine Service / Mercator Ocean International), PSY4 (Copernicus Marine Service / Mercator Ocean International), and GLO12 et PSY4 forecasts.
[2] IPCC AR6 SYR chapter 4.3 https://www.ipcc.ch/report/ar6/syr/downloads/report/IPCC_AR6_SYR_LongerReport.pdf