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El Niño in Monterey Bay

The bay right now against normal. Explanations follow the numbers.

200 ft down (M1, 60 m)

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Surface water at the bay buoys

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Sea above the tide table

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Bay surface vs normal (satellite)

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Solid lines are measured. Dashed lines are the normal for the time of year.

The El Niño signal 200 ft down

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The 60 m normal is the 2018–2025 average for this week, worked out by us from the mooring's own 2018 to 2025 record: a short baseline, not a 30-year climate normal. M1 data

What El Niño is

El Niño is the warm phase of a natural climate pattern across the tropical Pacific. It comes and goes irregularly, every two to seven years on average, and can affect weather around the world. NOAA Climate.gov

The Pacific in a normal year and an El Niño yearNormal yearThermoclineWarm waterCold deep waterWestEastAsia, AustraliaSouth AmericaTrade windsCold upwellingEl Niño yearThermoclineWarm waterCold deep waterWestEastAsia, AustraliaSouth AmericaWeak trade winds

In a normal year the trade winds blow west along the equator, from South America toward Asia. They pile warm surface water up in the western Pacific, so the thermocline (the boundary between warm surface water and cold deep water) sits deep in the west and slopes up toward the east, where cold water rises near South America. NOAA NOAA PMEL

In an El Niño year the trade winds weaken. Warm water is pushed back east toward the Americas, the thermocline flattens (it sinks in the east and rises in the west), and upwelling brings less cold water to the surface in the east. NOAA NOAA PMEL

Monterey Bay in cross-section

Monterey Bay in cross-sectionNormalThermoclineOffshoreShore0 m60 m150 mWind from the north, along the coastSurface water pushed offshoreUpwellingCold, nutrient-richM1 mooring60 m (200 ft)El NiñoThermoclineOffshoreShore0 m60 m150 mWind from the north, along the coastSurface water pushed offshoreUpwellingWarmer, fewer nutrientsM1 mooring60 m (200 ft)

In summer, winds blow from the north along the coast. They push surface water offshore, and cold, nutrient-rich water rises from below to take its place. This is upwelling. The nutrients fertilize the surface water, which is why upwelling coasts are rich in life. NOAA NOAA

This year the thermocline has deepened. That pushes the nutrient-rich water below the depth upwelling reaches, so upwelled water is warmer and poorer in nutrients. MBARI

On 26 Oct 2026 MBARI's M1 mooring measured 64.7 °F (18.18 °C) at 60 m (about 200 ft) down, beating the record set on 19 Nov 1997 in an earlier El Niño. MBARI MBARI's data show temperatures more than 7 °C (12.6 °F) above the long-term average. MBARI

What it changes here

Warm-water visitors have turned up: a winged comb jelly and a rose siphonophore west of Davidson Seamount, schools of halfmoon fish at M1, juvenile pelagic red crabs, and a quick glimpse of several Humboldt squid. MBARI

What comes next

  1. Now

    El Niño reaches the bay

    By late October 2026 El Niño had reached Monterey Bay, with record-warm water about 200 ft down. MBARI

  2. Winter

    The warmest water

    El Niño brings the warmest water to the bay in winter. MBARI

  3. Spring

    The strongest biological effects

    MBARI expects the strongest biological effects in spring. MBARI

  4. After

    The effects linger for months

    The warmest water comes in winter, but the effects linger for several months. MBARI

This is what MBARI expects, not a forecast of ours.

Sources and further reading

60 m water temperature: MBARI M1 mooring via CeNCOOS. Buoy water temperatures: NOAA NDBC. Tide gauge: NOAA CO-OPS Monterey 9413450. Free to use with credit; we add nothing to the measurements.

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