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The Tide Between Us: An Irish-Caribbean Story of Slavery & Emancipation (The O'Neill Trilogy Book 1)

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The first Irish emigrants to Jamaica arrived more than 200 years previous to my Jamaican friend’s 1850 ancestors. In 1641, Ireland’s population was 1,466,000 and in 1652, 616,000. According to Sir William Petty, 850,000 were “wasted by the sword, plague, famine, hardship and banishment during the Confederation War 1641-1652.” At the end of the war, vast numbers of Irish men, women and children were forcibly transported by the English government. Medieval understanding of the tides was primarily based on works of Muslim astronomers, which became available through Latin translation starting from the 12th century. [23] Abu Ma'shar al-Balkhi (d. circa 886), in his Introductorium in astronomiam, taught that ebb and flood tides were caused by the Moon. [23] Abu Ma'shar discussed the effects of wind and Moon's phases relative to the Sun on the tides. [23] In the 12th century, al-Bitruji (d. circa 1204) contributed the notion that the tides were caused by the general circulation of the heavens. [23] The semi-diurnal range (the difference in height between high and low waters over about half a day) varies in a two-week cycle. Approximately twice a month, around new moon and full moon when the Sun, Moon, and Earth form a line (a configuration known as a syzygy [9]), the tidal force due to the Sun reinforces that due to the Moon. The tide's range is then at its maximum; this is called the spring tide. It is not named after the season, but, like that word, derives from the meaning "jump, burst forth, rise", as in a natural spring. The first tide table in China was recorded in 1056 AD primarily for visitors wishing to see the famous tidal bore in the Qiantang River. The first known British tide table is thought to be that of John Wallingford, who died Abbot of St. Albans in 1213, based on high water occurring 48 minutes later each day, and three hours earlier at the Thames mouth than upriver at London. [40]

Simon Stevin, in his 1608 De spiegheling der Ebbenvloet ( The theory of ebb and flood), dismissed a large number of misconceptions that still existed about ebb and flood. Stevin pleaded for the idea that the attraction of the Moon was responsible for the tides and spoke in clear terms about ebb, flood, spring tide and neap tide, stressing that further research needed to be made. [24] [25]Tidal constituents are the net result of multiple influences impacting tidal changes over certain periods of time. Primary constituents include the Earth's rotation, the position of the Moon and Sun relative to the Earth, the Moon's altitude (elevation) above the Earth's Equator, and bathymetry. Variations with periods of less than half a day are called harmonic constituents. Conversely, cycles of days, months, or years are referred to as long period constituents. Her third novel, The Weaver's Legacy, tells the story of an Irish Catholic colony in the American West from 1866 to 1937. Tidal forces affect the entire earth, but the movement of solid Earth occurs by mere centimeters. In contrast, the atmosphere is much more fluid and compressible so its surface moves by kilometers, in the sense of the contour level of a particular low pressure in the outer atmosphere. Migration to Jamaica continued through the 17th century. The term Redleg was coined. The fair skin of the Irish frazzled beneath the Caribbean sun. The Irish exiles were not chattel slaves. Their white skin meant they would know freedom when their indenturship expired.

Pierre-Simon Laplace formulated a system of partial differential equations relating the ocean's horizontal flow to its surface height, the first major dynamic theory for water tides. The Laplace tidal equations are still in use today. William Thomson, 1st Baron Kelvin, rewrote Laplace's equations in terms of vorticity which allowed for solutions describing tidally driven coastally trapped waves, known as Kelvin waves. [32] [33] [34] A beautiful novel that's full of forbidden passions, family secrets and a lot of courage and sacrifice.”—Reese WitherspoonYears later I watched the Jamaican movie Cool Runnings. Only when the credits rolled, I noticed the Irish surnames, Roche, McLaughlin, Crowe, Morrison, Maloney, Harris. A few years later I watched a documentary on Bob Marley and noted a peculiar Irish lilt in some of the words spoken by the Jamaicans. Most of us born in Ireland pre-1990 will have attended a Catholic school, sat beside a white Irish child, taken a white boy or girl to our debs and had little to no interaction with people other than Irish, Catholic and white. As a “blow-in” to the rural town I was as foreign as it got. The tidal force produced by a massive object (Moon, hereafter) on a small particle located on or in an extensive body (Earth, hereafter) is the vector difference between the gravitational force exerted by the Moon on the particle, and the gravitational force that would be exerted on the particle if it were located at the Earth's center of mass. It was thought that the Irish would have a better chance of survival if they were introduced to the climate at a young age. Cromwell then sent 2,000 children between the age of 10 and 14 years.

Her first novel, The Memory of Music tells the story of one family during Ireland's most turbulent years, the 1916 uprising and the subsequent War of Independence and Civil War. It is one of the few novels to explore the role of women. It was the winner of the Annie McHale Best Debut and remained in the Bestselling Charts for 3 months. The Naturalis Historia of Pliny the Elder collates many tidal observations, e.g., the spring tides are a few days after (or before) new and full moon and are highest around the equinoxes, though Pliny noted many relationships now regarded as fanciful. In his Geography, Strabo described tides in the Persian Gulf having their greatest range when the moon was furthest from the plane of the Equator. All this despite the relatively small amplitude of Mediterranean basin tides. (The strong currents through the Euripus Strait and the Strait of Messina puzzled Aristotle.) Philostratus discussed tides in Book Five of The Life of Apollonius of Tyana. Philostratus mentions the moon, but attributes tides to "spirits". In Europe around 730 AD, the Venerable Bede described how the rising tide on one coast of the British Isles coincided with the fall on the other and described the time progression of high water along the Northumbrian coast. When the Moon is at first quarter or third quarter, the Sun and Moon are separated by 90° when viewed from the Earth, and the solar tidal force partially cancels the Moon's tidal force. At these points in the lunar cycle, the tide's range is at its minimum; this is called the neap tide, or neaps. "Neap" is an Anglo-Saxon word meaning "without the power", as in forðganges nip (forth-going without-the-power). [11] As the Earth rotates, the magnitude and direction of the tidal force at any particular point on the Earth's surface change constantly; although the ocean never reaches equilibrium—there is never time for the fluid to "catch up" to the state it would eventually reach if the tidal force were constant—the changing tidal force nonetheless causes rhythmic changes in sea surface height.Writing is a solitary process. Do you have a routine so that you don’t get completely lost in the world(s) you are creating? When the new heirs to the plantation arrive from Ireland they resurrect the ghosts of brutal injustices against Art. He bides his time and hides his abhorrence from his new master by channeling his energy into his work. During those years he prospers, he acquires land, he sees his coloured children freed after emancipation as he takes us on a multi-generational historical saga. Eventually Art is promised seven gold coins for seven decades of service. He doubts his master will part with the coins. The morning Art sets out to claim his gratuity, he ignores his sense of foreboding that he may not return home alive. Maclaurin used Newton's theory to show that a smooth sphere covered by a sufficiently deep ocean under the tidal force of a single deforming body is a prolate spheroid (essentially a three-dimensional oval) with major axis directed toward the deforming body. Maclaurin was the first to write about the Earth's rotational effects on motion. Euler realized that the tidal force's horizontal component (more than the vertical) drives the tide. In 1744 Jean le Rond d'Alembert studied tidal equations for the atmosphere which did not include rotation. Tidal phenomena are not limited to the oceans, but can occur in other systems whenever a gravitational field that varies in time and space is present. For example, the shape of the solid part of the Earth is affected slightly by Earth tide, though this is not as easily seen as the water tidal movements. The changing distance separating the Moon and Earth also affects tide heights. When the Moon is closest, at perigee, the range increases, and when it is at apogee, the range shrinks. Six or eight times a year perigee coincides with either a new or full moon causing perigean spring tides with the largest tidal range. The difference between the height of a tide at perigean spring tide and the spring tide when the moon is at apogee depends on location but can be large as a foot higher. [12] Other constituents

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