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Science / News report

A cold bay can sit beside a warmer Pacific

Kachemak’s survey compares water layers, not interchangeable temperatures.

Event / announcement date
2026-10-28
Bay, forest and mountains viewed from Homer.
File photo: Kachemak Bay from Homer, September 30, 2006; not a temperature measurement. · “Kachemak Bay, Alaska” — Hobig / Public domain · Unchanged source raster. · Image source ↗ · public-domain ↗

NOAA’s October 28 Kachemak Bay account reports colder-than-normal September subsurface water despite widespread North Pacific surface warming. Local surface temperatures had approached average conditions in August. The measurements describe different depths and places. [1]

A conductivity-temperature-depth instrument records changes through the water column. NOAA’s instrument guide explains that comparing temperature and salinity helps identify water masses; a surface map cannot supply the entire vertical profile. [2]

Monthly surveys began in 2012. Some March 2026 measurements fell below 1°C after a cold winter. Comparing repeated stations with seasonal averages revealed local persistence; broader surface conditions cannot describe every depth. [1]

CTD profiles help investigate marine-life distributions. Readers comparing ocean reports should check sampling depth, location and reference period. [2]

The source

  1. NOAA NCCOS: Kachemak Bay temperature profiles ↗
    Source date 2026-10-28 · reviewed October 29, 2026
  2. NOAA Ocean Exploration: Conductivity temperature and depth ↗
    Source date 2020-06-22 · reviewed October 29, 2026 · No publication date is given on this reference.
Sources reviewed October 29, 2026. External pages may change.

About this item: News report. No first-hand reporting or independent testing is claimed. Corrections policy.

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