Skip to main content

What a Falling Glass Does to the Water

, 6 min read

A falling barometer is a messenger. The front behind it changes wind, light, temperature, and runoff, and those are the changes fish meet in the water.

The mercury, or the aneroid capsule, or the number on a phone, is one of the oldest weather instruments anglers still argue about. A falling glass, a hard high, a swing of ten hectopascals in a day: the language of the barometer is part of fishing talk from piers to pike lakes. The instrument is measuring the weight of the air column above you. What arrives with a change in that weight is a weather front, and a front does a lot of work on the water.

This piece follows that work: wind, light, temperature, runoff, and then the difference between the pressure fish feel with depth and the pressure of the air.

What is a falling glass announcing?

Air has mass. At sea level the column of atmosphere typically presses at about 1013 hPa. A deepening low, often the approach of a front, lowers that number. A building high raises it. The number on its own is a label for the air mass. The weather that travels with the air mass is the event.

A falling glass in temperate latitudes often means a low and its fronts are on the way: wind increasing and changing direction, cloud thickening, rain or a dump of river water later, a shift in air temperature, and, on a coast, a change in wave height and in how hard the surface mixes. A rising glass after the front often means clearing skies, a shift toward a quieter wind, colder nights in winter, hotter still days in summer.

Anglers who say “the pressure shut them down” are usually remembering the whole package. The package is worth unpacking.

How does a front change wind and mixing?

Wind is the first hand on the water. It piles water onto one bank, strips the other, and stirs the surface. On a shallow lake that stirring resuspends silt and can mix oxygen downward. On a stratified lake in summer a strong blow can tilt the thermocline or, in smaller waters, delay the layering. On a coast it builds or kills a surf, dirties a sandy shore, and changes how a rip runs.

A front often swings the wind through 90 or 180 degrees in a few hours. Fish that were using a lee shore lose it. Bait that was held in a slick is scattered. The same swing can turn a dead, glassy lake into a coloured, oxygenated one. That is a feeding change with a mechanical cause. The barometer moved in the same hours because the same low moved the wind.

How does light and temperature move with the front?

Cloud is the second hand. Thick frontal cloud cuts the light in the water. Sight-feeders that were working a bright shallows may drop a little deeper or wait. Species that hunt in lower light, or in stained water, may start. After the front, a hard high can bring a bluebird sky. Clear, stable air over clear water is a difficult noon for many predators, especially in winter when the Sun is already low.

Air temperature rides along. A warm sector ahead of a front can lift the surface of a shallow lake a degree or two in a day. A cold clearance behind it can strip that heat overnight. Fish are cold-blooded; even a small swing in the water they sit in changes how often they need to eat. The glass fell, then rose. The heat budget of the lake did the biological work.

What does runoff do after the rain?

Many fronts bring rain. Rain on a clay or agricultural catchment turns a river the colour of tea in an afternoon and pushes a plume of fresh, dirty, sometimes colder water into a lake or an estuary. Turbidity shortens how far a pike can see. Salinity at a river mouth drops. Extra nutrients can feed an algal bloom days later.

The barometer has already bottomed and started up by the time the river peaks. If you only watch the glass, you miss the delayed dirt. If you watch the colour of the water, you are reading the front’s real gift to the fish.

Do fish feel air pressure?

They feel pressure constantly, because water is heavy. Every ten metres of depth adds about one atmosphere, roughly 1013 hPa, of hydrostatic pressure. A perch that moves from two metres to four metres has doubled the pressure on its body from the water, a change of about 200 hPa. A weather system that drops the air by 20 hPa is a small fraction of that, spread over hours.

Fish have a swim bladder and other sensors that register pressure, and they use depth as a place to sit. A 20 hPa swing at the surface is real. It is also tiny next to a two-metre change in depth, which a fish can make in seconds. The physiology supports “fish notice pressure.” It is a long walk from there to a favourite number on a kitchen barometer.

Where air pressure is most plausible as a cue is as a coincident label: the hours when wind, light, temperature, and runoff are already changing. Trend then matters more than the absolute 1013. A rapid fall says a front is close. The question to ask next is which of the water’s properties is moving with it.

What is worth watching on the day?

Look at the water the front is touching. Has the wind mixed or dirtied it? Has the light dropped under cloud, or gone harsh under a new high? Has the surface temperature stepped? Has a river coloured the mark, or will it tomorrow? On the coast, has the swell and the run changed with the same system?

The glass is a useful messenger. The message is the weather arriving in the water.

barometric-pressurefishing-forecastresearchfish-behaviour