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Effects	of	the	El	Niño	Weather	System	on	Fish	Populations	Off	the	Peruvian	Coast	
	
Tyler	Franzen	
	
November	22nd	2015
Introduction	
Every	two	to	seven	years	our	planet	goes	through	changes	in	its	weather	system	known	as	
El	Niño.			An	El	Niño	weather	event	is	known	to	have	a	“bubble”	of	warm	ocean	water	that	
develops	in	the	central	and	east–central	equatorial	Pacific	right	off	the	coast	of	South	America	
(Laws,	2000).		El	Niño	is	part	of	the	El	Nino	Southern	Oscillation	or	ENSO	for	short	(Evers	2011).		
ENSO	is	a	cycle	of	warm	and	cold	sea	surface	temperatures	or	SST	of	the	central	and	eastern	
Pacific	Ocean	(McPhaden,	2001).		El	Niño	is	caused	by	high	air	pressure	in	the	western	Pacific	and	
low	air	pressure	in	the	eastern	Pacific	
(Laws,	2000).		When	the	ENSO	is	not	in	
an	El	Niño	phase	(warm	phase)	it	is	in	a	
La	Niña	phase	(cool	phase)	with	sea	
surface	temperatures	in	the	Eastern	
Pacific	below	average	and	air	pressures	
are	higher	in	the	eastern	Pacific	and	
lower	in	the	western	Pacific	(Evers,	
2011).		In	most	years,	winds	from	the	
southeast	push	warm	surface	water	
away	from	the	coast	known	as	upwelling	(Evers,	2011).		Upwelling	brings	cold-water	rich	
nutrients	to	the	surface	(McPhaden,	2001).		Every	so	often	(two	to	seven	years)	the	pattern	of	air	
circulation	of	the	equatorial	Pacific	changes	in	a	way	that	alters	the	normal	oceanic	upwelling.	
During	these	years	warm	water	is	being	pushed	towards	the	surface	instead	of	the	usual	nutrient	
rich	cold	water	(McPhaden,	2001).		During	El	Nino,	the	upwelling	brings	up	warm	water	with	very	
few	nutrients,	which	results	in	devastating	economic	consequences	to	fishing	industries	off	the	
Figure	1:	This	graph	shows	the	ENSO	cold	and	warm	SST	
phases	The	University	of	Washington	recorded	from	1950	to	
the	year	2000.		(McPhaden,	2001)
coast	of	Peru	and	Chili,	this	is	especially	true	in	the	Anchovy	fisheries	(Salmon,	2015).			Large	
populations	of	fish	and	sea	birds	fall	victim	of	El	Niño	and	vanish	while	this	weather	system	is	
present.		If	Peru	does	not	constantly	regulate	fishing,	especially	during	El	Niño	years,	there	may	
not	be	enough	fish	to	repopulate	in	the	years	following.	Currently	Peru	puts	restrictions	on	the	
length	(in	weeks)	of	the	two	fishing	seasons	as	well	as	the	tonnage	of	fish	caught	per	Fishery	and	
the	total	for	the	season.	
	
Cascade	effect	
El	Niño	affects	manyof	the	countries	bordering	the	Pacific	Ocean,	and	a	large	portion	of	
these	countries	depend	heavily	on	fishing	every	year.		Fishermen	in	the	area	noticed	that	the	ENSO	
weather	pattern	many	years	ago	
and	coined	the	term	"El	Niño"	
which	is	a	reference	to	the	Christ	
child	because	periodic	warming	in	
the	Pacific	near	South	America	is	
often	noticed	around	Christmas.	
"La	Niña",	chosen	as	the	'opposite'	
of	El	Niño,	simply	translates	to	
"The	Girl"(Salmon,	2015).		
Plankton	is	the	typical	food	source	
for	many	fish	including	Peru’s	primary	catch,	the	anchovy	(Laws,	2000).		Fishermen,	and	later	
scientists,	have	attributed	poor	fishing	years	due	to	the	absence	of	plankton	(Salmon,	2015).		
Figure	2:	Annual	catch	of	Peruvian	anchovies	from	1950	to	the	year	2000.		
Note	that	years	with	low	yield	correspond	to	years	that	had	an	El	Niño	
event.	(Hannesson,	2001)
When	there	is	a	warm	water	upwelling	off	the	South	American	Pacific	Coast	the	plankton	do	not	
have	an	adequate	amount	of	nutrients	from	the	warm	water	to	thrive,	thus	is	also	affecting	all	
species	that	are	higher	up	in	the	food	chain	(Salmon,	2015).		
	
Prevention	or	Economic	Devastation	
Fishing	is	the	second	largest	industry	in	Peru	behind	mineral	and	oil	extraction	(Gaulter,	
2015).		With	that	being	said,	any	change	in	the	annual	fishing	rates	will	alter	the	countries	
economic	portfolio	immensely.		When	there	are	years	without	large	amounts	of	fish	caught,	the	
country	struggles	economically	(Gaulter,	2015).		If	you	did	a	side-by-side	comparison	of	figure	one	
and	two	you	would	see	a	strong	correlation	between	annual	catch	of	Peruvian	fish	and	sea	surface	
temperatures	(SST)	(Laws,	2000).		Years	with	a	high	SST	will	have	lower	catch	rates	and	vice	versa	
(Laws,	2000).		In	1972	to	1973	there	was	a	strong	El	Niño	event	that	left	fish	populations	critically	
low	for	quite	a	few	years	into	the	future	(Salmon,	2015).		Some	scientists	are	concerned	that	
overfishing	during	El	Niño	weather	systems	along	with	large	fish	and	seabirds	also	feeding	on	the	
smaller	fish	like	the	anchovy	that	recover	after	such	an	episode	would	be	very	long	and	difficult	if	
not	impossible	(Laws,	2000).		Thankfully,	after	the	1972	episode	the	Peruvian	government	
enacted	many	laws	in	regards	to	fishing	especially	in	years	undergoing	an	El	Niño	episode	(Laws,	
2000).		These	laws	have	successfully	prevented	several	fish	wipeout	events	from	taking	place	in	
Peruvian	territorial	waters	such	as	the	El	Niño	episode	in	1988-1989	(Laws,	2000).		Even	with	
preventative	measure	in	place,	wipeout	events	may	still	take	occur,	thus	the	Peruvian	government	
must	remain	wary	and	proactive	(Gaulter,	2015)
Conclusion	
	 El	Niño	has	global	impacts	not	only	with	fishing	but	also	weather	patterns	such	as	rain	and	
snowfall,	humidity,	and	even	air	temperatures	due	to	changes	in	jet	streams.		Today	we	can	
predict	with	much	certainty	when	El	Niño	events	will	occur.	This	helps	fisheries	and	governments	
prepare	for	these	events	so	economies	don’t	collapse	and	crops,	that	do	better	during	El	Niño	
weather	conditions,	can	be	planted	during	those	seasons	(Gaulter	2015).		If	governments	do	not	
regulate	fisheries	properly,	overfishing	can	quickly	lead	to	years	and	years	of	low	fish	counts	after	
such	an	episode.		Illegal	fishing	has	become	a	major	problem	in	South	America	but	local	
governments	are	increasing	ocean	patrols	to	combat	such	activities.	Overall,	laws	and	regulations	
have	become	much	more	suited	to	these	El	Niño	events	over	the	past	thirty	years	and	thus	have	
kept	overfishing	in	check.	This	allows	the	fisheries	to	go	about	as	usual	much	sooner	after	an	El	
Niño	episode	than	if	these	laws	were	not	in	place	and	properly	enforced.		The	Peruvian	
government	does	a	good	job	of	combating	the	ill	effects	of	these	ENSO	events	but	there’s	only	so	
much	it	can	do	given	that	we	cannot	control	plankton	populations	during	warm	water	phases.	
Countries	can	only	control	the	length	of	the	fishing	season	and	caps	on	how	many	fish	can	be	
caught	during	these	seasons.		Overall,	ENSO	events	have	global	impacts,	but	the	real	effects	are	
seen	in	countries	such	as	Peru,	where	fishing	is	a	major	part	of	their	economic	portfolio	and	even	
slight	changes	can	largely	affect	the	nations	GDP.
Bibliography	
Evers,	J.	(Ed.).	(2011,	March	11).	El	Niño	-	El	Niño-Southern	Oscillation	(ENSO).	Retrieved	
November	19,	2015,	from	http://education.nationalgeographic.org/encyclopedia/el-nino/	
Gaulter,	S.	(2015,	July	26).	El	Nino's	effect	on	Peru.	Retrieved	November	19,	2015,	from	
http://www.gulf-times.com/environment/231/details/448730/el-nino’s-effect-on-peru	
Hannesson,	R.	(2001,	November	1).	A	Note	On	Unsustainable	Fisheries	And	Trends	In	World	Fish		
Catches.	Retrieved	November	19,	2015,	from	
http://www.fao.org/docrep/005/y3684e/y3684e05.htm	
Laws,	E.	(2000).	El	Niño	and	the	Peruvian	Anchovy	Fishery.	Retrieved	November	20,	2015,	from
	 http://www.ucar.edu/communications/gcip/m12anchovy/m12html.html	
McPhaden,	M.,	&	Soreide,	N.	(2001).	NOAA/PMEL/TAO	Frequently	asked	Questions	about	El	Nino	
and	La	Nina.	Retrieved	November	19,	2015,	from	
http://www.pmel.noaa.gov/tao/elnino/nino-home.html	
Salmon,	P.	(2015,	May	11).	ENSO	and	the	anchovy.	Retrieved	November	19,	2015,	from		
	 http://judithcurry.com/2015/05/11/enso-and-the-anchovy/

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