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MY'STORY

The MOVE Fire

This is a personal recollection on the Move fire on May 13, 1985 Philadelphia police fired thousands of rounds at the MOVE house, city officials approved dropping an explosive device on the roof, the resulting fire was allowed to burn, 11 people—including five children—died, and 61 homes were destroyed. Philadelphia City Council later called it a “brutal attack carried out by the City of Philadelphia on its own citizens” and acknowledged that no individual faced criminal consequences for the bombing. One timeline correction worth preserving for the BHP record: the major previous MOVE-police confrontation was August 8, 1978, about seven years before the bombing, not a year or two earlier. Officer James Ramp was killed, other police and firefighters were wounded, nine MOVE members were later convicted, and television cameras recorded police beating Delbert Africa during his arrest. The 1985 MOVE Commission later specifically criticized city planners for failing to adequately use lessons from that 1978 confrontation. And that actually strengthens the point you’re making: 1985 did not happen without precedent or institutional memory. There had already been a deadly confrontation with MOVE, years of conflict, negotiations and police involvement before Osage Avenue.

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BLACK FACTS
The Truths They Never Taught You...

Shirley Chisholm — Unbought and Unbossed

In 1968 Shirley Chisholm became the first Black woman elected to the United States Congress. In 1972 she launched a campaign for the Democratic presidential nomination, breaking another political barrier.

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BHP gathered finds from its connected research sources. Showing the 4 strongest Black History matches.
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Wikipedia

Sea state

NOAA ship Delaware II in foul weather on Georges Bank.
Sea State 5 and 8 range

In oceanography, 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 spectrum. The sea state varies with time, as the wind and swell conditions change. The sea state can be assessed either by an experienced observer (like a trained mariner) or by using instruments like weather buoys, wave radar, or Earth observation satellites.[1]

The short-term statistics describing the sea state are determined for a time interval in which the sea state is considered to be constant. This duration has to be much longer than the individual wave period, but shorter than the period in which the wind and swell conditions can be expected to vary significantly. Typically, the sea state is assumed to be constant for 15-30 minutes.[1]

The large number of variables involved in creating and describing 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.[citation needed]

WMO sea state code

[edit]
Winter, North Atlantic – Water over deck and hatches, storm with huge waves (1958)

The World Meteorological Organization (WMO) sea state code largely adopts the 'wind sea' definition of the Douglas Sea Scale.[citation needed] The direction from which the swell is coming should be recorded.[citation needed]

graphic of WMO sea state codes, descriptions, and wave heights in meters
WMO Sea State Code Wave height Characteristics
0 0 metres (0 ft) Calm (glassy)
1 0 to 0.1 metres (0.0 to 3.9 in) Calm (rippled)
2 0.1 to 0.5 metres (3.9 in to 1 ft 7.7 in) Smooth (wavelets)
3 0.5 to 1.25 metres (1 ft 8 in to 4 ft 1 in) Slight
4 1.25 to 2.5 metres (4 ft 1 in to 8 ft 2 in) Moderate
5 2.5 to 4 metres (8 ft 2 in to 13 ft 1 in) Rough
6 4 to 6 metres (13 to 20 ft) Very rough
7 6 to 9 metres (20 to 30 ft) High
8 9 to 14 metres (30 to 46 ft) Very high
9 Over 14 metres (46 ft) Phenomenal
Character of the sea swell
  0. None
Low 1. Short or average
2. Long
Moderate 3. Short
4. Average
5. Long
High 6. Short
7. Average
8. Long
  9. Confused

Sea states in marine engineering

[edit]

In engineering applications, sea states are often characterized by the following two parameters:

In addition to the short-term wave statistics presented above, long-term sea state statistics are often given as a joint frequency table of the significant wave height and the mean wave period. From the long and short-term statistical distributions, it is possible to find the extreme values expected over a given number of years by fitting an extreme value distribution.[3] The extreme value distribution can then inform an engineer about the most extreme significant wave height to be expected during the lifetime of a ship or offshore structure. Using the response amplitude operators of the ship, the engineer can then use the extremes in significant wave height and wave period to calculate the most extreme loads that the ship should be able to withstand. Withstanding significant wave heights that happen on average once in 100 years or once in 1000 years is a common demand for design of ships and offshore structures.[4]

CCI Sea State

[edit]

The "Sea State" project within the ESA's Climate Change Initiative (CCI) program created an 18-year data set (2002–2020) covering various sea state-related Essential Climate Variables as measured by the Jason satellite series, other ocean-focused Earth observation satellites, and in situ sources.[5][6][7][8] In 2025, data from CCI Sea State, combined with the new SWOT satellite measurements, were used to describe a new record wave height of nearly 20 m in the open ocean.[9][10]

See also

[edit]

Citations

[edit]
  1. ^ a b Holthuijsen, Leo H. (2007). Waves in oceanic and coastal waters. Cambridge: Cambridge University Press. ISBN 978-0-511-27021-5.
  2. ^ Munk, W.H. (1944). Proposed uniform procedure for observing waves and interpreting instrument records. La Jolla, California: Wave Project at the Scripps Institution of Oceanography.
  3. ^ Aarnes, Ole Johan; Breivik, Øyvind; Reistad, Magnar (2012). "Wave Extremes in the Northeast Atlantic". Journal of Climate. 25 (5): 1529–1543. doi:10.1175/JCLI-D-11-00132.1. hdl:1956/9253. ISSN 0894-8755.
  4. ^ Jonathan, Philip; Ewans, Kevin (2013). "Statistical modelling of extreme ocean environments for marine design: A review". Ocean Engineering. 62: 91–109. doi:10.1016/j.oceaneng.2013.01.004.
  5. ^ "Sea State". ESA Climate Office. Retrieved 2025-10-11.
  6. ^ "CCI Sea State". Laboratory for Ocean Physics and Satellite remote sensing. Retrieved 2025-10-11.
  7. ^ Laboratory, Plymouth Marine. "Sea State CCI". Plymouth Marine Laboratory. Retrieved 2025-10-11.
  8. ^ "CCI+ Sea State". www.dlr.de. Retrieved 2025-10-11.
  9. ^ "Satellites reveal the power of ocean swell". www.esa.int. Retrieved 2025-10-11.
  10. ^ Ardhuin, Fabrice; Postec, Taina; Accensi, Mickael; Piolle, Jean-François; Dodet, Guillaume; Passaro, Marcello; De Carlo, Marine; Husson, Romain; Guitton, Gilles; Collard, Fabrice (2025-09-23). "Sizing the largest ocean waves using the SWOT mission". Proceedings of the National Academy of Sciences. 122 (38) e2513381122. doi:10.1073/pnas.2513381122. PMC 12478040. PMID 40956893.

General and cited references

[edit]

Source: Wikipedia. Article content is retrieved live through the MediaWiki API.

Wikipedia

Sea state

In oceanography, 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 spectrum. The sea state varies with time, as the wind and swell conditions change. The sea state can be assessed either by an experienced observer (like a trained mariner) or by using instruments like weather buoys, wave radar, or Earth observation satellites. The short-term statistics describing the sea state are determined for a time interval in which the sea state is considered to be constant. This duration has to be much longer than the individual wave period, but shorter than the period in which the wind and swell conditions can be expected to vary significantly. Typically, the sea state is assumed to be constant for 15-30 minutes. The large number of variables involved in creating and describing 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.

MORE →
Wikipedia

Red Sea State

Red Sea State (Arabic: ولاية البحر الأحمر, Wilāyat al-Baḥr al-ʾAḥmar) is one of the 18 wilayat (states) of Sudan. It covers an area of about 218,887 km2 and has an estimated population of 1.48 million. The state borders Egypt to the north, River Nile State to the west, Kassala State to the south, Eritrea to the southeast, and the Red Sea to the east. Its capital and largest city is Port Sudan, which serves as Sudan's main seaport and handles around 90% of the country's international trade, making the state Sudan's only maritime outlet to the Red Sea and the Indian Ocean. Much of Sudan's coastline lies within Red Sea State, giving it strategic and economic importance, and more than half of its population lives in urban areas. Sudan also claims the Halaib Triangle on the northern frontier as part of Red Sea State, although the area is administered by Egypt and remains the subject of an ongoing territorial dispute.

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Wikipedia

Salton Sea State Recreation Area

The Salton Sea State Recreation Area offers hunting, fishing, swimming, and camping to visitors on the northeastern side of the Salton Sea.

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Wikipedia

Kassala State

Kassala (Arabic: ولاية كسلا, called Ash Sharqiyah during 1991–1994) is one of the 18 wilayat (states) of Sudan. It has an area of 36,710 km2 and an estimated population of approximately 2,519,071 in 2018. The state borders Khartoum to the west, Qadarif to the south, Eritrea to the east, River Nile to the northwest, and Red Sea State to the northeast. Kassala is the capital of the state. Towns in the state of Kassala include Aroma, Hamashkoraib, Halfa el Jadida (New Halfa), Khashm el Girba and Telkuk. In 2016, Kassala State suffered a severe bread shortage.

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TOPIC OF THE DAY

Greenwood / Black Wall Street

Before the 1921 destruction of Tulsa’s Greenwood District, Black residents had created a remarkable center of business and community life. The district included stores, professional offices, entertainment venues and homes owned by Black citizens. Understanding Greenwood means learning what was built—not only what was burned.

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TRIVIA QUESTION OF THE DAY

Which Supreme Court case ruled state-sponsored public-school segregation unconstitutional?

Brown v. Board of Education in 1954.