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El Niño and the Galápagos

This is a guest post by Prof. Kris Karnauskas of the University of Colorado Boulder. He runs the Oceans and Climate Lab (@OceansClimateCU), which aims to improve the understanding the tropical ocean and atmosphere, its interaction with ecosystems, and how it has changed in the past and will change in the future. In his spare time we hear he runs ultra-marathons, which is simultaneously very cool and kind of crazy.

What happens when a tiny island rises from the seafloor and stands directly in the path of one of the grandest ocean currents in the world? This happened millions of years ago, when the Galapagos Archipelago formed. We now have penguins in the tropics and such a remarkable biological system that it got Darwin thinking about life. There is far more than one could learn in a lifetime about geology, ecology, biology, and evolution from the Galápagos, partly because of where they are on the planet. In fact, it is precisely where the islands just happened to have formed—smack on the equator—that makes them so fascinating and important.

 

20,000 leagues under the sea

Imagine you could see miles beneath the surface of the sea, revealing highways of currents in every direction—sometimes even stacked on top of one other. In the tropical Pacific, you would notice the Equatorial Undercurrent flowing eastward some 8,000 miles, all the way from Papua New Guinea toward South America—about a third of the way around the planet.

This current is centered at a depth near 150-650 feet across most of the Pacific and rises up (upwells) toward the surface near South America. It moves at a top speed of a little over 3 mph (just a casual walking pace), which doesn’t sound very impressive. However, multiplying by its width and height reveals that about 10 billion gallons of cold water are moving by every second!

The Equatorial Undercurrent was discovered accidently in the early 1950s, when long-line fishermen noticed their gear drifting eastward beneath their boat—the opposite direction as the wind and surface current. Now we know it’s a fundamental part of the global ocean circulation.

Penguins and fur seals and tortoises, oh my

The Galápagos formed on the equator some millions of years ago in the eastern Pacific. The largest island (Isabela) extends from about 1.1°S to 0.2°N. Isla Isabela quite literally forms a wall in the ocean that just happens to have the same dimensions as the Equatorial Undercurrent barreling toward it from the west. Some of the water manages to sneak around the islands, while some rises up to the surface.

 

The cold water in the deep ocean is full of nutrients. When it rises up into the sunlight, it fuels photosynthesis and a remarkable abundance of phytoplankton, the basic food for much of the ocean ecosystem. This food source has allowed the Galapagos to develop into a unique outpost of biodiversity. Virtually all of the penguins and fur seals live along the western shores of Isabela and Fernandina (Boersma, 1977; Vargas et al., 2005, 2006) where the upwelling is strongest and water temperatures are measurably cooler than elsewhere in the vicinity.

 

There is another source of upwelling waters in the Galapagos: the trade winds, which normally blow from east to the west on either side of the equator. These winds push water generally westward and away from the equator. Cold water from the deep ocean rises up to replace it. The Galápagos sit right in the middle of the tongue of cold water that results from the wind-driven upwelling.

SSTs in July 2014

Sea surface temperatures in July 2014 (an ENSO-neutral period), showing the tongue of cold water that extends across the eastern tropical Pacific when the trade winds are blowing normally. The trade winds relax during El Niño, and the cold tongue subsides. NOAA Climate.gov map from Data Snapshots.

 

But then El Niño comes along

What happens when nature throws a wrench in this delicate balance of physics and biology? During an El Niño event, the Galápagos is geographically positioned in the heart of the warming ocean waters. (See this map of October 2015, for example.) The change in water temperatures can affect the marine life directly. Upwelling from the Equatorial Undercurrent, for instance, is reduced during an El Niño, reducing the food supply in the near-surface waters. Also, during El Niño, the trade winds are weakened, so that source of upwelling is reduced. In other words, El Niño is a double-whammy for the Galápagos, doing away with the broader wind-driven upwelling and the Equatorial Undercurrent.

 

Precipitous declines in the Galapagos penguin population have followed past major El Niño events, including 1982-83 and 1997-98. Penguin population collapses during or following major El Niño events are understandable from an oceanographic perspective. The Equatorial Undercurrent weakens substantially and even disappears altogether during such events (Firing et al., 1983), with dramatic consequences for the entire food web from schooling fish to penguins (Boersma, 1978 and 1998; Boersma et al., 2013, fur seals (Aurioles and Trillmich, 2008), marine iguanas (Nelson et al., 2004), and other marine predators.

 

The most amazing thing to me is still the coincidence of the islands; had they formed a degree north or south of where they did, none of this would matter. The Galápagos would not stand in the way of the Equatorial Undercurrent; consequently, the local oceanographic conditions (and the ecology that depends on them) would be fundamentally different. Upon stepping off the HMS Beagle in 1835, what biota would Charles Darwin have found, and how might that have influenced contemporary thought, philosophy, religion, and the development of evolutionary biology? It is this fluke of geography that helped create such abundant biodiversity in the Galápagos, but also the islands vulnerability to Earth’s great climatic heartbeat, El Niño.

Lead reviewer: Michelle L'Heureux

Primary References

Karnasuskas, K. Dispatches from Paris: Galápagos vs. the greatest ocean current in the world

Karnauskas, K. B., R. Murtugudde, and W. B. Owens, 2014: Climate and the Global Reach of the Galápagos Archipelago: State of the Knowledge, in The Galápagos: A Natural Laboratory for the Earth Sciences (eds K. S. Harpp, E. Mittelstaedt, N. d'Ozouville and D. W. Graham), John Wiley & Sons, Inc, Hoboken, New Jersey, doi: 10.1002/9781118852538.ch11.

Karnauskas, K. B., S. Jenouvrier, C. W. Brown, and R. Murtugudde, 2015: Strong sea surface cooling in the eastern equatorial Pacific and implications for Galápagos Penguin conservation. Geophys. Res. Lett., 42(15), 6432-6437, doi: 10.1002/2015GL064456.

Additional References

Aurioles, D., and F. Trillmich (2008), Arctocephalus galapagoensis, The IUCN Red List of Threatened Species (2014.3).

Boersma, P. D. (1977), An ecological and behavioral study of the Galápagos Penguin, Living Bird, 15, 43–93.

Boersma, P. D. (1978), Breeding patterns of Galápagos Penguins as an indicator of oceanographic conditions, Science, 200, 1481–1483.

Boersma, P. D. (1998), Population trends of the Galápagos Penguin: Impacts of El Niño and La Niña, Condor, 100(2), 245–253.

Boersma, P. D., A. Steinfurth, G. Merlen, G. Jiménez–Uzcátegui, F. Vargas, and P. G. Parker (2013), Galápagos Penguin (Spheniscus mendiculus), in Penguins Natural History and Conservation, edited by P. G. Borboroglu and P. D. Boersma, 360 pp., Univ. of Washington Press, Seattle, Wash. [Available at www.washington.edu/uwpress/search/books/BORPEN.html.]

Firing, E., R. Lukas, J. Sadler, and K. Wyrtki (1983), Equatorial Undercurrent disappears during 1982–1983 El Niño, Science, 222(4628), 1121–1123.

Nelson, K., H. Snell, and M. Wikelsi (2004), Amblyrhynchus cristatus, The IUCN Red List of Threatened Species (Version 2014.3).

Vargas, H., C. Lougheed, and H. Snell (2005), Population size and trends of the Galápagos Penguin Spheniscus mendiculus, Ibis, 147(2), 367–374.

Vargas, F. H., S. Harrison, S. Rea, and D. W. Macdonald (2006), Biological effects of El Niño on the Galápagos Penguin, Biol. Conserv., 127(1), 107–114.

Vargas, F. H., R. C. Lacy, P. J. Johnson, A. Steinfurth, R. J. M. Crawford, P. D. Boersma, and D. W. Macdonald (2007), Modelling the effect of El Niño on the persistence of small populations: The Galápagos Penguin as a case study, Biol. Conserv., 137(1), 138–148.

Comments

I have been pondering a possible connection between El Nino and the genetic composition of an animal population. When an event causes a population crash, the genetic quality of the population can improve because more of the "less fit" don't survive. Is it possible that the population crashes caused by super El Ninos are a key contributor to the biodiversity on the Galapagos? Each time the population crashes the "fittest" make up a greater proportion of the surviving population, effectively putting evolution into hyper drive? I came to this question when considering the genetic "quality" of the New Zealand dairy herd. New Zealand is facing a major drought (from this year's El Nino) and farmers are reducing their stocking numbers. New Zealand has one of the best databases of cow genetics in the world and so most NZ farmers are including cow genetic ranking when selecting cows to exit their herds. This means the genetic "quality" of the national herd would improve following the drought - provided adequate nutrition and care is provided for the cows that are retained. I then imagined how this would play out in a natural environment that is extraordinarily exposed to El Nino, like the Galapagos... Belinda Storey @nouveaueco

I appreciated the article on the Galapagos. I am curious as to what the current affects of El Nino are on the Galapagos? Are the affects greater at this time due the strength of this year's El Nino, or do the affects on plant and animal populations occur later in spring. Many thanks, Ed

how can we stop el nino. It makes me sad.

I don't think there is any way to stop it during our lifetimes. The amount of heat energy involved is mingboggling. It would be a little like asking how we can change the rotation rate of the earth, so we can have 25-hour days instead of 24, to have more time each day. A bunch of ants cannot move a house from one corner of the block to the other.

In reply to by Amy Coghlin

when did el nino hit the galapagos islands

Hi Isobel,

Since El Ninos occur in the central and eastern equatorial Pacific Ocean and affect the circulation along the entire equator, whenever there is any El Nino, it likely will have some sort of impact on the Galapagos Islands. Although, not all El Ninos will have the same impact. The stronger the El Nino and the farther east the abnormally warm ocean temperatures occur along the equator, the more likely the impact is larger.

The last El Nino was in 2015-2016.

In reply to by Isobel

Both events: El Niño (warm) and La Niña (cold) dramatically affect Galapagos Island whole ecosystem (marine and land). Your article really good.

Your article was excellent and very easy to understand. Just one point. There are sea lions in Galapagos, not seals.  Sea lions have external ears, seals do not. Likewise Fur sea lions are in Galapagos, not Fur seals.

Well, we're definitely not marine mammal biologists here at the ENSO blog. I do know the thing about the internal versus external ears, but perhaps this was a situation where the common name came to be used before those taxonomic differences were fully understood?

All I can say is that there are some pinnipeds (which is a word I just love, btw) that are widely referred to as "fur seals" despite their greater similarity to sea lions. And indeed, according to the website of the Galapagos Conservation Trust, the islands actually have both a "Galapagos fur seal" and a "Galapagos sea lion"! 

https://galapagosconservation.org.uk/fur-seal-or-sea-lion/

Are you saying you think our picture is of the sea lion, not the fur seal?

 

In reply to by Michele Adler

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