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Marine Weather Lab

An interactive visual lesson for clouds, fronts and weather charts.

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Weather-chart field guide

Clouds

Cirrus

High cloud

Delicate white strands, hooks, or silky streaks. These ice clouds look feathered, with no rounded cauliflower tops.

  • Fine fibres and wind-swept hooks
  • Thin strands with blue sky between them

Weather clue: Often seen ahead of changing weather; their presence alone does not predict rain.

Compare with Cirrostratus: Cirrus forms separate streaks. Cirrostratus spreads into a more continuous veil.

WMO field reference

Cirrocumulus

High cloud

A high field of tiny white grains or ripples. From the ground the small elements have little or no grey shading.

  • Very small, regularly arranged cloudlets
  • Usually no visible shading from the ground

Weather clue: A useful sign of structure in high-level air; rain generally does not reach the surface from these clouds.

Compare with Altocumulus: More than 30° above the horizon, cirrocumulus elements usually appear less than 1° wide. Altocumulus elements usually appear 1–5° wide and show shading.

WMO field reference

Cirrostratus

High cloud

A pale, translucent veil of ice crystals. It can cover much of the sky while the Sun remains visible.

  • Smooth or finely fibrous veil
  • A halo around the Sun or Moon is a useful clue

Weather clue: May accompany an approaching weather system. A halo is a clue to ice crystals, not a forecast by itself.

Compare with Altostratus: Cirrostratus commonly produces a halo. Altostratus dims the Sun like frosted glass without a halo.

WMO field reference

Altocumulus

Middle cloud

Rounded patches or rolls in a mid-level layer. White tops and grey shading give the cloudlets a textured appearance.

  • Repeated rounded patches, often in rows
  • Some grey shading beneath the elements

Weather clue: Some forms indicate instability aloft; the genus alone cannot tell you whether storms will develop.

Compare with Cirrocumulus: From the ground, these elements usually look larger and more shaded than cirrocumulus.

WMO field reference

Altostratus

Middle cloud · can extend higher

A broad grey-blue sheet. In thinner parts, the Sun looks blurred, as though seen through frosted glass.

  • A fairly uniform grey or bluish layer
  • A dim Sun, with no halo

Weather clue: Can thicken as a weather system approaches; precipitation may develop as the layer deepens.

Compare with Cirrostratus: Altostratus is thicker and greyer than cirrostratus, and does not produce a halo.

WMO field reference

Nimbostratus

Middle cloud · often extends into other levels

A thick, dark layer with a diffuse, rainy base. Its continuous cover hides the Sun; ragged fragments may hang below.

  • Widespread, fairly continuous precipitation
  • Thick cover with an indistinct underside

Weather clue: Associated with persistent rain or snow, rather than the brief showers typical of convective clouds.

Compare with Cumulonimbus: Nimbostratus spreads into a rain layer. Cumulonimbus builds a tower, often with an anvil.

WMO field reference

Stratocumulus

Low cloud

A low blanket made of large rounded masses or rolls. Darker bases and bright edges create a lumpy layer.

  • Large, rounded masses joined into a layer
  • Grey bases, sometimes with gaps of blue

Weather clue: Often brings overcast skies; drizzle or light precipitation is possible.

Compare with Cumulus: Stratocumulus spreads sideways into joined rolls. Cumulus more often forms separate, upright heaps.

WMO field reference

Stratus

Low cloud

A low, fairly featureless grey blanket. Its base is much smoother than the rolling texture of stratocumulus.

  • A low, nearly uniform layer
  • Few distinct tops or rounded elements

Weather clue: May bring drizzle. Low stratus can obscure elevated terrain and reduce visibility where it meets the ground.

Compare with Stratocumulus: Stratus is smoother. Stratocumulus has recognisable rounded masses or rolls.

WMO field reference

Cumulus

Low base · vertical growth

Bright heaps with a flat base. Look for crisp, rounded tops separated by blue sky.

  • Puffed, cauliflower-like tops
  • A distinct flat, often darker base

Weather clue: Small cumulus often accompanies fair weather. Increasing vertical growth suggests stronger convection.

Compare with Stratocumulus: Cumulus grows into separate upright heaps. Stratocumulus spreads into a lower, joined layer.

WMO field reference

Cumulonimbus

Low base · deep vertical growth

A massive cloud tower reaching high into the atmosphere. Its upper part becomes fibrous and may spread into an anvil.

  • Strong vertical development
  • A fibrous upper region, often anvil-shaped

Weather clue: Associated with thunderstorms, heavy showers, and sometimes hail or strong gusts.

Compare with Nimbostratus: Look for a deep tower and a spreading top, rather than a uniform rain-bearing sheet.

WMO field reference
Fronts

Warm front

Chart symbol: A red line carrying solid semicircles. The semicircles bulge towards the direction the front is travelling.

Approach

Warm air replaces cooler air and rises gradually over it. Cloud and precipitation often spread ahead of the surface front, giving useful signs before passage, but the pattern varies with the system.

Passage

In this illustrative sequence, rain eases and temperature rises near passage. In real cases the pressure, wind, precipitation and temperature changes depend on the front’s strength and local conditions.

Behind it

Air behind the front is often warmer and more humid. Low cloud, mist or drizzle may persist; visibility depends on moisture, wind and sea temperature.

Sailor’s signs

  • Barometer: pressure often falls ahead and steadies or rises after passage; the rate varies.
  • Wind: in a Northern Hemisphere depression it may back before passage and often veer as the front crosses; direction and amount vary.
  • Temperature: it often rises behind a warm front, but the size and timing vary.
  • Visibility: it may fall in precipitation or frontal fog where warm rain moistens cooler air.
  • Sea state: a swell may arrive before local wind changes, depending on the storm’s fetch.

What to do

  • Prepare the vessel and crew before conditions deteriorate, using the current forecast and the vessel’s procedures.
  • Fix your position and log it before visibility closes in.
  • Log pressure regularly and compare its trend with the current forecast and other observations.
  • Allow for a possible wind shift when reviewing the passage plan.

Risks

  • Long hours of rain and closed visibility with a crew that is already tired.
  • Sea fog in the warm sector, over a cold sea, right when you want to make a landfall.
  • A lee shore becoming dangerous as the wind builds hours before the front arrives.

Cold front

Chart symbol: A blue line carrying solid triangles. The triangles point the way the front is travelling.

Approach

Cooler, denser air undercuts warmer air. A narrow band of showers or thunderstorms may occur near the front, but precipitation can be ahead, behind or absent.

Passage

In this illustrative sequence, passage brings a sharp wind shift and heavy showers. Real cold fronts range from weak to squall-producing.

Behind it

Air behind is often cooler and drier; showers and improved visibility may follow, but conditions depend on the air mass and sea temperature.

Sailor’s signs

  • Barometer: the fall often stops and pressure begins to rise; timing and magnitude vary.
  • Wind: a marked shift is common near a cold front in the Northern Hemisphere, but its direction and size depend on the pressure pattern.
  • Temperature: it often falls behind the front, but the change may be small or delayed.
  • Visibility: showers can reduce visibility, with clearer intervals possible between them.
  • Sea state: a cross sea may develop when the new wind meets the earlier swell.

What to do

  • Prepare for possible squalls before the cloud band arrives; available warning time varies.
  • Secure the vessel and use the appropriate crew safety equipment before conditions worsen.
  • Choose sail trim and steering for the vessel, point of sail, sea room and conditions; there is no universal squall manoeuvre.
  • Allow for a possible veer, and avoid letting the new wind put you on a lee shore.

Risks

  • A violent gust and wind shift together, which is how boats are knocked down and gear is broken.
  • A confused cross sea for several hours after the passage.
  • Hail, lightning and near-zero visibility in the squall itself.

Occluded front

Chart symbol: A purple line with semicircles and triangles alternating on the same side, both pointing the way the front is travelling.

Approach

A cold front can catch a warm front and lift the warm sector away from the surface. The air masses determine whether the occlusion has more warm-front or cold-front character.

Passage

The fronts may appear as one band. Rain, showers, wind change and pressure response vary; embedded convection can occur within the cloud and precipitation.

Behind it

Conditions often improve gradually, but an occlusion can resemble either a warm or a cold front. Cloud, rain and temperature changes depend on the air masses.

Sailor’s signs

  • Barometer: pressure may be near a local minimum and then rise, but the pattern depends on the depression.
  • Wind: a change may occur, with direction and timing set by the surrounding pressure pattern and air masses.
  • Temperature: the change can be small when similar cool air masses meet, or more marked in another occlusion.
  • Visibility: precipitation and cloud may reduce it; improvement depends on the band’s structure and wind.
  • Sea state: an older swell can remain after the depression starts to fill.

What to do

  • Do not assume a warm sector; a missing temperature rise can support an occlusion diagnosis when other signs agree.
  • Allow for a potentially prolonged rain band and manage crew fatigue.
  • Maintain a proper lookout and use radar when fitted and operational; embedded showers can contain squalls.
  • Check the forecast and observations before judging that conditions are improving; a pressure rise alone is insufficient.

Risks

  • A long exposure to rough conditions that wears down the crew rather than testing them briefly.
  • Embedded cumulonimbus hidden inside a uniform rain shield.
  • A false clearance: the sky brightens, then the next band arrives.

Stationary front

Chart symbol: Alternating red semicircles on one side of the line and blue triangles on the other, each pointing at the air mass it is failing to displace.

Approach

Neither air mass advances decisively. Winds can run along the boundary and cloud or precipitation may persist, but the structure and duration vary from case to case.

Passage

There may be no clear passage. Conditions on one side can continue while waves or disturbances develop along the boundary.

Behind it

There is no defined “behind” until the boundary moves or a wave develops. A new disturbance can change the weather quickly.

Sailor’s signs

  • Barometer: it may remain nearly steady, but a wave can introduce a clear fall or rise.
  • Wind: it can run parallel to the front; direction and change depend on the local pressure pattern.
  • Temperature: it may remain stable on one side while contrasting air lies nearby.
  • Visibility: cloud or precipitation can keep it moderate or poor along the boundary.
  • Sea state: it can build with fetch and duration even without a frontal passage.

What to do

  • Monitor the pressure pattern and observations; little frontal movement does not guarantee unchanged weather.
  • Watch for a wave developing along the boundary; some waves deepen into depressions.
  • Review the forecast and available sea room before relying on a persistent wind direction.
  • Keep logging pressure; a new tendency may signal a changing pressure pattern.

Risks

  • Days of rain and poor visibility with no improvement to sail towards.
  • A frontal wave deepening quickly into a new low right on top of you.
  • Complacency, because nothing has changed for two days.

Sources

Weather charts

How to read this weather chart

Each contour joins equal pressure. Closer contours mean a stronger pressure gradient; the central L or H is a reference. Around a low, air circulates inward and friction crosses the isobars. Without a course, the barometer samples a stationary vessel position; with a course, it follows the vessel along the displayed passage.

Focus a marker and use arrow keys; hold Shift for a larger step.

Arrows show where air goes · wind direction is named from where it comes

This lesson uses synthetic Gaussian systems with fixed teaching parameters: 70% surface-wind speed and a 15° cross-isobar friction turn. Curvature and local effects are omitted, so this is a schematic teaching chart rather than a forecast or routing product.