Jan Umsonst
https://www.facebook.com/taoist.attack/posts/3422485977881946 ·
A look on the Southern Ocean marine heatwaves - doesn't look good, as they are also intensifying...
Our main problem: ocean heat uptake remained even during the El Nino 2023/24 on record levels - insane the numbers of the last years!
Important for this post: During La Ninas the oceans take up much more heat than during El Ninos.
The central to eastern tropical Pacific being colder than normal during La NInas supports ocean heat uptake over the abnormal cold areas. During El Ninos the opposite happens as the oceans loose vast amounts of heat to the atmosphere during El Ninos when the central to eastern tropical Pacific is warmer than normal.
The high rates of ocean heat uptake during the triple La Nina from 2020 to 2022 are thought to be one reason behind the exceptional ocean surface warming during 2023/24. Some of the take up heat resurfaced into the upper mixed layer during 2023/24 which caused this exceptional surface warming signal. The El Nino in 2023/24 played here a large role.
Still the signal of heat resurfacing had been exceptional.
But now we have the problem that ocean heat uptake did not decline or reversed during 2023/24 when we had the last El Nino emitting vast amounts of energy into the atmosphere.
The rates of ocean heat uptake had been similar in 2023/24 to 2020-22, which should not be possible, at least not back on back...
Lets talk about numbers...
The numbers of ocean heat uptake (IAP/CAS dataset) in 2021 of 15Zj, 2022 of 19Zj, 2023 of 16Zj and 2024 of 16ZJ (1) have to be seen in relation to these numbers:
Regardless of which estimate is used, there has been a two- to three- fold increase in the rate of increase in OHC since the late 1980s. For example, according to the IAP analy- sis, the OHC trend for 1958–1985 is 3.1 ± 0.5 ZJ yr−1, and since 1986, the OHC trend is 9.2 ± 0.5 ZJ yr−1 (Fig. 2). The IAP trend within 1958–1985 of 3.1 ± 0.5 ZJ yr−1 is higher than the previous release in Cheng et al. (2023) (2.3 ± 0.5 ZJ yr−1), mainly because the new inclusion of the bottle data bias correction. After 2007, with better global coverage of ocean subsurface data, OHC uncertainty is reduced. There is a significant warming trend of 10.8 ± 1.2 ZJ yr−1 and 10.3 ± 0.8 ZJ yr−1 from 2007–2023 for IAP/CAS and NCEI/NOAA (seasonal time series), respectively (Fig. 2). The NCEI three-month OHC estimate has a slightly stronger trend than the pentadal time series from 2005 to 2020, indicating the impact of sam- pling changes associated with the mapping approach. (2)
(1) New Record Ocean Temperatures and Related Climate Indicators in 2023";
https://link.springer.com/article/10.1007/s00376-024-3378-5(2) "Record High Temperatures in the Ocean in 2024";
https://link.springer.com/.../10.1007/s00376-025-4541-3...These studies are important for what happens in the oceans (read them in the order):
(1) "New Record Ocean Temperatures and Related Climate Indichttps://link.springer.com/article/10.1007/s00376-024-3378-5
(2) "A Glimpse into the Future: The 2023 Ocean Temperature and Sea Ice Extremes in the Context of Longer-Term Climate Change ";
https://journals.ametsoc.org/.../105/3/BAMS-D-23-0209.1.xml(3) "Record High Temperatures in the Ocean in 2024";
https://link.springer.com/.../10.1007/s00376-025-4541-3...(4) "Quantifying the acceleration of multidecadal global sea surface warming driven by Earth's energy imbalance";
https://iopscience.iop.org/article/10.1088/1748-9326/adaa8a"Drivers of the 2023 record shattering marine heat extreme in the North Atlantic";
https://www.researchsquare.com/article/rs-5046018/v1