SEA STATE

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Sea state In oceanography, a sea state is the general condition of the free surface on a large body of water—with respect to wind waves and swell—at a certain location and moment. A sea state is characterized by statistics, including the wave height, period, and power spectrum. The sea state varies with time, as the wind conditions or swell conditions change. The sea state can either be assessed by an experienced observer, like a trained mariner, or through instruments like weather buoys, wave radar or remote sensing satellites. In case of buoy measurements, the statistics are determined for a time interval in which the sea state can be considered to be constant. This duration has to be much longer than the individual wave period, but smaller than the period in which the wind and swell conditions vary significantly. Typically, records of one hundred to thousand wave-periods are used to determine the wave statistics. The large number of variables involved in creating the sea state cannot be quickly and easily summarized, so simpler scales are used to give an approximate but concise description of conditions for reporting in a ship's log or similar record World Meteorological Organization sea state code The WMO sea state code largely adopts the 'wind sea' definition of the Douglas Sea Scale . WMO Sea State Code Wave Height (meters) Characterist ics 0 0 Calm (glassy) 1 0 to 0.1 Calm (rippled)

Transcript of SEA STATE

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Sea stateIn oceanography, a sea state is the general condition of the free surface on a large body of water

—with respect to wind waves and swell—at a certain location and moment. A sea state is

characterized by statistics, including the wave height, period, and power spectrum. The sea state

varies with time, as the wind conditions or swell conditions change. The sea state can either be

assessed by an experienced observer, like a trained mariner, or through instruments like weather

buoys, wave radar or remote sensing satellites.

In case of buoy measurements, the statistics are determined for a time interval in which the sea

state can be considered to be constant. This duration has to be much longer than the individual

wave period, but smaller than the period in which the wind and swell conditions vary

significantly. Typically, records of one hundred to thousand wave-periods are used to determine

the wave statistics.

The large number of variables involved in creating the sea state cannot be quickly and easily

summarized, so simpler scales are used to give an approximate but concise description of

conditions for reporting in a ship's log or similar record

World Meteorological Organization sea state code

The WMO sea state code largely adopts the 'wind sea' definition of the Douglas Sea Scale.

WMO Sea State CodeWave Height

(meters)Characteristics

0 0 Calm (glassy)

1 0 to 0.1 Calm (rippled)

2 0.1 to 0.5 Smooth (wavelets)

3 0.5 to 1.25 Slight

4 1.25 to 2.5 Moderate

5 2.5 to 4 Rough

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6 4 to 6 Very rough

7 6 to 9 High

8 9 to 14 Very high

9 Over 14 Phenomenal

Character of the sea swell

  0. None

Low1. Short or average2. Long

Moderate3. Short4. Average5. Long

Heavy6. Short7. Average8. Long

  9. Confused

Direction from which swell is coming should be recorded.

Confused swell should be recorded as "confused northeast," if coming from the direction

of northeast.

Beaufort scaleThe Beaufort scale is an empirical measure that relates wind speed to observed conditions at sea

or on land. Its full name is the Beaufort Wind Force Scale.

History

The scale was devised in 1805 by Sir Francis Beaufort, an Irish-born Royal Navy Officer, while

serving on HMS Woolwich. The scale that carries Beaufort's name had a long and complex

evolution, from the previous work of others, including Daniel Defoe the century before, to when

Beaufort was a top administrator in the Royal Navy in the 1830s when it was adopted officially

and first used during Darwin's voyage on HMS Beagle.[1] In the early 19th Century, naval

officers made regular weather observations, but there was no standard scale and so they could be

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very subjective - one man's "stiff breeze" might be another's "soft breeze". Beaufort succeeded in

standardizing the scale.

The initial scale of thirteen classes (zero to twelve) did not reference wind speed numbers but

related qualitative wind conditions to effects on the sails of a man-of-war, then the main ship of

the Royal Navy, from "just sufficient to give steerage" to "that which no canvas sails could

withstand."[2] At zero, all his sails would be up; at six, half of his sails would have been taken

down; and at twelve, all sails would be stowed away.[3]

The scale was made a standard for ship's log entries on Royal Navy vessels in the late 1830s and

was adapted to non-naval use from the 1850s, with scale numbers corresponding to

cup anemometer rotations. In 1916, to accommodate the growth of steam power, the descriptions

were changed to how the sea, not the sails, behaved and extended to land observations. Rotations

to scale numbers were standardized only in 1923. George Simpson, Director of the

UKMeteorological Office, was responsible for this and for the addition of the land-based

descriptors.[1] The measure was slightly altered some decades later to improve its utility

for meteorologists. Today, many countries have abandoned the scale and use the metric-based

units m/s or km/h instead,[citation needed] but the severe weather warnings given to public are still

approximately the same as when using the Beaufort scale.

The Beaufort scale was extended in 1946, when Forces 13 to 17 were added. [4] However, Forces

13 to 17 were intended to apply only to special cases, such as tropical cyclones. Nowadays, the

extended scale is only used in Taiwan and mainland China, which are often affected by

typhoons.

Wind speed on the 1946 Beaufort scale is based on the empirical formula:[5]

v = 0.836 B3/2 m/s

where v is the equivalent wind speed at 10 metres above the sea surface and B is Beaufort

scale number. For example, B = 9.5 is related to 24.5 m/s which is equal to the lower limit of

"10 Beaufort". Using this formula the highest winds in hurricanes would be 23 in the scale.

Today, hurricane force winds are sometimes described as Beaufort scale 12 through 16, very

roughly related to the respective category speeds of the Saffir-Simpson Hurricane Scale, by

which actual hurricanes are measured, where Category 1 is equivalent to Beaufort 12.

However, the extended Beaufort numbers above 13 do not match the Saffir-Simpson Scale.

Category 1 tornadoes on the Fujita and TORRO scales also begin roughly at the end of level

12 of the Beaufort scale but are indeed independent scales.

Note that wave heights in the scale are for conditions in the open ocean, not along the shore.

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The modern scale

Beaufort

number

DescriptionWind speed

Wave

height

Sea conditions Land conditions Sea state photoAssociated Warning

Flag

0 Calm

< 1 km/h (< 0.3 m/s) 0 m

Flat.Calm. Smoke rises vertically.

< 1 mph

< 1 kn

0 ft

< 0.3 m/s

1 Light air

1.1–5.5 km/h (0.3–2 m/s) 0–0.2

m

Ripples without crests.

Smoke drift indicates wind direction and wind vanes cease moving.

1–3 mph

1–2 kn

0–1 ft

0.3–1.5 m/s

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2 Light breeze

5.6–11 km/h (2–3 m/s) 0.2–

0.5 m

Small wavelets. Crests of glassy appearance, not breaking

Wind felt on exposed skin. Leaves rustle and wind vanes begin to move.

4–7 mph

3–6 kn

1–2 ft

1.6–3.4 m/s

3 Gentle breeze

12–19 km/h (3–5 m/s)

0.5–1 m

Large wavelets. Crests begin to break; scattered whitecaps

Leaves and small twigs constantly moving, light flags extended.

8–12 mph

7–10 kn

2–3.5 ft

3.4–5.4 m/s

4 Moderate breeze

20–28 km/h (6–8 m/s)

1–2 m

Small waves with breaking crests. Fairly frequent whitecaps.

Dust and loose paper raised. Small branches begin to move.

13–17 mph

11–15 kn

3.5–6 ft

5.5–7.9 m/s

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5 Fresh breeze

29–38 km/h (8.1-10.6 m/s) 2–3

m

Moderate waves of some length. Many whitecaps. Small amounts of spray.

Branches of a moderate size move. Small trees in leaf begin to sway.

18–24 mph

16–20 kn

6–9 ft

8.0–10.7 m/s

6 Strong breeze

39–49 km/h (10.8-13.6 m/s) 3–4

m

Long waves begin to form. White foam crests are very frequent. Some airborne spray is present.

Large branches in motion. Whistling heard in overhead wires. Umbrella use becomes difficult. Empty plastic garbage cans tip over.

25–30 mph

21–26 kn

9–13 ft

10.8–13.8 m/s

7 High wind,Moderate gale,Near gale

50–61 km/h (13.9-16.9 m/s)

4–5.5 m

Sea heaps up. Some foam from breaking waves is blown into streaks along wind direction. Moderate amounts of airborne spray.

Whole trees in motion. Effort needed to walk against the wind.

31–38 mph

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27–33 kn

13–19 ft

13.9–17.1 m/s

8 Gale,Fresh gale

62–74 km/h (17.2-20.6 m/s) 5.5–

7.5 m Moderately high waves with breaking crests forming spindrift. Well-marked streaks of foam are blown along wind direction. Considerable airborne spray.

Some twigs broken from trees. Cars veer on road. Progress on foot is seriously impeded.

39–46 mph

34–40 kn

18–25 ft

17.2–20.7 m/s

9 Strong gale

75–88 km/h (20.8-24.4 m/s) 7–10

m High waves whose crests sometimes roll over. Dense foam is blown along wind direction. Large amounts of airborne spray may begin to reduce visibility.

Some branches break off trees, and some small trees blow over. Construction/temporary signs and barricades blow over.

47–54 mph

41–47 kn

23–32 ft

20.8–24.4 m/s

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10 Storm,[6]

Whole gale

89–102 km/h (24.7-28.3 m/s)

9–12.5 m

Very high waves with overhanging crests. Large patches of foam from wave crests give the sea a white appearance. Considerable tumbling of waves with heavy impact. Large amounts of airborne spray reduce visibility.

Trees are broken off or uprooted, saplings bent and deformed. Poorly attached asphalt shingles and shingles in poor condition peel off roofs.

55–63 mph

48–55 kn

29–41 ft

24.5–28.4 m/s

11 Violent storm

103–117 km/h (28.6-32.5 m/s) 11.5–

16 mExceptionally high waves. Very large patches of foam, driven before the wind, cover much of the sea surface. Very large amounts of airborne spray severely reduce visibility.

Widespread damage to vegetation. Many roofing surfaces are damaged; asphalt tiles that have curled up and/or fractured due to age may break away completely.

64–72 mph

56–63 kn

37–52 ft

28.5–32.6 m/s

12 Hurricane Force[6]

≥ 118 km/h (≥ 32.8 m/s)

≥ 14 m

Huge waves. Sea is completely white with foam and spray. Air is filled with driving spray, greatly reducing visibility.

Very widespread damage to vegetation. Some windows may break; mobile homes and poorly constructed sheds and barns are damaged. Debris may be hurled about.≥

73 mph

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≥ 64 kn

≥ 46 ft≥

32.7 m/s

The scale is used in the Shipping Forecasts broadcast on BBC Radio 4 in the United

Kingdom, and in the Sea Area Forecast from Met Éireann, the Irish Meteorological Service.

Met Éireann issues a "Small Craft Warning" if winds of Beaufort Force 6 (min. mean of 22

knots) are expected up to 10 Nautical miles offshore. Other warnings are issued by Met

Éireann for Irish coastal waters, which are regarded as extending 30 miles out from the

coastline, and the Irish Sea or part thereof: "Gale Warnings" are issued if winds of Beaufort

Force 8 are expected; "Strong Gale Warnings" are issued if winds of Beaufort Force 9 or

frequent gusts of at least 52 knots are expected.; "Storm Force Warnings" are issued if

Beaufort Force 10 or frequent gusts of at least 61 knots are expected; "Violent Storm Force

Warnings" are issued if Beaufort Force 11 or frequent gusts of at least 69 knots are expected;

"Hurricane Force Warnings" are issued if winds of greater than 64 knots are expected.

This scale is also widely used in Greece, China, Taiwan, Hong Kong and Macau, however

with some differences between them. Taiwan uses the Beaufort scale with the extension to

17 noted above. China also switched to this extended version without prior notice on the

morning of 15 May 2006,[7] and the extended scale was immediately put to use for Typhoon

Chanchu. Hong Kong and Macau however keep using Force 12 as the maximum.

In the United States, winds of force 6 or 7 result in the issuance of a small craft advisory,

with force 8 or 9 winds bringing about a gale warning, force 10 or 11 a storm

warning ("a tropical storm warning" being issued instead of the latter two if the winds relate

to a tropical cyclone), and force 12 a hurricane force wind warning (or hurricane warning if

related to a tropical cyclone). A set of red warning flags (daylight) and red warning lights

(night time) is displayed at shore establishments which coincide with the various levels of

warning.

In Canada, maritime winds forecast to be in the range of 6 to 7 are designated as "strong"; 8

to 9 "gale force"; 10 to 11 "storm force"; 12 "hurricane force". Appropriate wind warnings

are issued by Environment Canada's Meteorological Service of Canada: strong wind

warning, gale (force wind) warning, storm (force wind) warning and hurricane force wind

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warning. These designations were standardized nationally in 2008, whereas "light wind" can

refer to 0 to 12 or 0 to 15 knots and "moderate wind" 12 to 19 or 16 to 19 knots, depending

on regional custom, definition or practice. Prior to 2008, a "strong wind warning" would

have been referred to as a "small craft warning" by Environment Canada, similar to US

terminology. (Canada and the USA have the Great Lakes in common.) However, there being

no generally accepted definition of "small craft", and to have consistency between wind

speed ranges and their associated warnings, the term "strong wind warning" has become the

national Canadian norm.

Cross seaIn surface navigation, a cross sea is a sea state with two wave systems traveling at oblique

angles.[1] This may occur when water waves from one weather system continue despite a shift

in wind. Waves generated by the new wind run at an angle to the old, creating a shifting,

dangerous pattern. Until the older waves have dissipated, they create a sea hazard among the

most perilous. A cross swell is generated when the wave systems are longer period swell, rather

than short period wind generated waves.