Guest “We don’t need no stinking null hypothesis” by David Middleton
Deadly marine ‘cold spells’ could become more frequent with climate change, scientists warn
Die-off in South Africa leads to investigation of changing ocean conditions
- 15 APR 2024
In March 2021, a grisly scene materialized on the beaches of South Africa. Giant bat-winged manta rays sprawled belly up on rocks. Hulking bull sharks lay dead in the sand. Puffer fish littered shorelines like deflated footballs.
Such fish kills are usually triggered by hot water, low oxygen, or toxic algae blooms. But this time it was a surprising culprit. In the middle of the southern summer, these fish died of cold—a phenomenon that may be linked to climate change, according to a new paper.
[…]
Weather and ocean conditions converged off South Africa with chilling results starting in late February 2021. Temperature data from satellites and buoys revealed that a large southbound eddy moving through the region, coupled with 4 days of strong easterly winds, fueled strong upwelling. Ocean surface temperatures along parts of the South African coast plunged by more than 7°C in 48 hours to as cold as 10°C. At one underwater temperature tracker near Port Alfred, on South Africa’s southeastern shore, temperatures fell by more than 9°C in a single day. The upwelling covered 230 kilometers of the ocean and lasted for a week.
[…]
It’s hard to say with certainty that the trend is driven by climate change, in part because these upwellings are so localized that they aren’t well represented in models looking at interactions between the ocean and climate, says David Schoeman, a marine climate change ecologist at the University of the Sunshine Coast who worked on the paper. But the trends are consistent with predictions of how climate change will…
Science
When every paradoxical observation is consistent with your hypothesis, it has become unfalsifiable and no longer retains a null hypothesis. This is whow hypotheses become quasi-religions.
The “new paper” is paywalled. Here’s the best line from the abstract:
Increasing upwelling could result in ‘bait and switch’ situations, where climate change expands subtropical species’ distribution, while simultaneously exposing climate migrants to an increased risk of cold-mortality events at poleward distributional limits.
Lubitz et al., 2024
Bait and Switch?
bait and switch
noun
1
: a sales tactic in which a customer is attracted by the advertisement of a low-priced item but is then encouraged to buy a higher-priced one
2
: the ploy of offering a person something desirable to gain favor (such as political support) then thwarting expectations with something less desirable
Merriam-Webster
Who would have ever guessed that the climate was capable of engaging in deceptive sales practices? Maybe it’s the climate “scientists” who are baiting and switching:
- “In March 2021, a grisly scene materialized on the beaches of South Africa. Giant bat-winged manta rays sprawled belly up on rocks. Hulking bull sharks lay dead in the sand. Puffer fish littered shorelines like deflated footballs.”
- “Weather and ocean conditions converged off South Africa with chilling results starting in late February 2021.”
- “It’s hard to say with certainty that the trend is driven by climate change…”
- “Deadly marine ‘cold spells’ could become more frequent with climate change, scientists warn”
Familiar pattern?
- Start with a negative observation (like lots of dead fish).
- Link it to a weather-related event.
- Postulate a link to climate change.
- Declare that future climate change will make this more frequent and/or worse.
The lame-stream media, UN bureaucrats, and left-wing politicians will blame every bad weather-related event on ExxonMobil and it will only get worse unless we undiscover fire and immediately forsake capitalism.
Upwelling and the El Niño-Southern Oscillation (ENSO)
What is upwelling?
Upwelling is a process in which deep, cold water rises toward the surface.
Winds blowing across the ocean surface push water away. Water then rises up from beneath the surface to replace the water that was pushed away. This process is known as “upwelling.”
Upwelling occurs in the open ocean and along coastlines. The reverse process, called “downwelling,” also occurs when wind causes surface water to build up along a coastline and the surface water eventually sinks toward the bottom.
Water that rises to the surface as a result of upwelling is typically colder and is rich in nutrients. These nutrients “fertilize” surface waters, meaning that these surface waters often have high biological productivity. Therefore, good fishing grounds typically are found where upwelling is common.
NOAA
While this example is for the Pacific Northwest USA, if there’s a global climate change effect on upwelling, it probably would show up here:
Upwelling Index
The Upwelling Index identifies the amount of surface water transported offshore using geostrophic wind approximations calculated from surface atmospheric pressure fields measured and reported by the U.S. Navy Fleet Numerical Meteorological and Oceanographic Center (FNMOC) in Monterey, California. The Upwelling Index can fluctuate yearly due to atmospheric shifts in pressure systems (Figure CU-02).
NOAA
Upwelling actually mitigates the effects of El Niño-driven ocean heat waves…
Abstract
Marine heatwaves are triggering coral bleaching events and devastating coral populations globally, highlighting the need to identify processes promoting coral survival. Here, we show that acceleration of a major ocean current and shallowing of the surface mixed layer enhanced localized upwelling on a central Pacific coral reef during the three strongest El Niño–associated marine heatwaves of the past half century. These conditions mitigated regional declines in primary production and bolstered local supply of nutritional resources to corals during a bleaching event. The reefs subsequently suffered limited post-bleaching coral mortality. Our results reveal how large-scale ocean-climate interactions affect reef ecosystems thousands of kilometers away and provide a valuable framework for identifying reefs that may benefit from such biophysical linkages during future bleaching events.
Fox et al., 2023 (Full text available)
Fox et al., 2023 demonstrated that over the past half-century, the effects of the three strongest El Niño-driven heat waves were mitigated by enhanced upwelling.
Lubitz et al, 2024 speculated that a climate change-related ocean heat wave caused localized upwelling and a “deadly marine cold spell,” killing lots of rays, puffer fish and bull sharks. Oddly enough, this “deadly marine cold spell” occurred early in the 2021-2023 La Niña:
And La Niña events are associated with the exact sort of upwelling (Benguela system, southwest coast) that Lubitz et al, 2024 tried to pin on climate change:
La Niña austral summers were associated with stronger upwelling favorable southeasterly winds and colder-than-normal coastal SST at the west and south coast of South Africa. In comparison, El Niño weakened the upwelling favorable southeasterly winds leading to less upwelling and warmer-than-normal coastal SST.
Rouault and Tomety, 2022 (Full text available)
While cold events in the Agulhas system (southeast coast) are local, driven by winds and currents and routinely caused “deadly cold spells”.
Abstract
Strong upwelling events inshore of the Agulhas Current close to 33.5°S are investigated. These events are important to the exchange of shelf and slope waters, potentially enhancing primary productivity and advecting larvae offshore. Using hydrographic observations, this study shows that a wind-driven upwelling event and a current-driven upwelling event can each advect central waters more than 130 m upward, resulting in a maximum 9°C cooling at 50-m depth over the continental shelf and surface cooling greater than 4°C. The authors use satellite data to assess the frequency and forcing mechanisms of similar cold events from January 2003 through December 2011, defining cold events as days when the sea surface temperature (SST) anomaly is significantly correlated with a local current or wind forcing. The authors identify 47 events with an average length of 2.2 days and SST anomaly of −1.6°C, corresponding to an average 13 days of surface cold events along the Agulhas Current front per year. This study uses combined EOF analysis to characterize these cold events based on four highly correlated forcing mechanisms: alongshore wind speed, wind stress curl, current meandering, and current speed over the slope. The authors find that meanders act in combination with upwelling-favorable winds to force the strongest cold events, while upwelling-favorable winds alone, possibly primed by Ekman veering, force weaker cold events. Most significantly, it is found that the frontal curvature of warm Agulhas Current meanders couples with the atmosphere to drive local wind stress curl anomalies that reinforce upwelling.
Leber et al., 2017 (full text available)
Leber et al., 2017 made no mention of climate change. Oddly enough, it was cited in Lubitz et al, 2024.
Real science leads to the conclusion that the “deadly marine cold spell” was related to the ENSO, local oceanographic & weather patterns, not terribly uncommon and that marine upwelling is normal and good. “Bait and switch science” speculates that the “deadly marine cold spell” was caused by anthropogenic global warming and that further use of fossil fuels will increase the frequency of such “grisly scene[s].”
References
Fox, Michael D. et al., Ocean currents magnify upwelling and deliver nutritional subsidies to reef-building corals during El Niño heatwaves.Sci. Adv.9,eadd5032(2023).DOI:10.1126/sciadv.add5032
Leber, G. M., L. M. Beal, and S. Elipot, 2017: Wind and Current Forcing Combine to Drive Strong Upwelling in the Agulhas Current. J. Phys. Oceanogr., 47, 123–134, https://doi.org/10.1175/JPO-D-16-0079.1.
Lubitz, N., Daly, R., Smoothey, A.F. et al. Climate change-driven cooling can kill marine megafauna at their distributional limits. Nat. Clim. Chang. (2024). https://doi.org/10.1038/s41558-024-01966-8
Rouault, M., and F. S. Tomety, 2022: Impact of El Niño–Southern Oscillation on the Benguela Upwelling. J. Phys. Oceanogr., 52, 2573–2587, https://doi.org/10.1175/JPO-D-21-0219.1.