913 research outputs found
The elegies of Ted Hughes
No full textThe purpose of this study is to make the case that Ted Hughes (1930-1998) is one of the pre-eminent elegists writing in English in the latter half of the twentieth century. Whilst his poetry has been widely criticised for its apparent preoccupation with violence and death, it is puzzling that the links these topics have in common with elegy have never been clearly verified. This might be because Hughes's elegies do not appear to bear the characteristics frequently associated with traditional poetic laments; however, as this study shows, closer scrutiny reveals not only many similarities, but also acts of resistance within the broader scope of elegy. Drawing on both established and contemporary critical debates surrounding Hughes and elegy, this study undertakes a comprehensive reading of the poet's major works from The Hawk in the Rain to Birthday Letters, whilst also paying attention to limited editions of his verse, including Recklings, Capriccio and Howls & Whispers. Posthumous publications, including the Collected Poems. Selected Translations and Letters of Ted Hughes, are accounted for. so that (alongside the chronological reading of the poems) Hughes's development as an elegist is fully realised. One of the aims of the thesis is to demonstrate that the poet's elegies are unified in presenting what I term the ‘actual'; that is to say, that Hughes does not fabricate sensations or forge experiences that purport to be beyond the realm of recognisable human endeavour. This I term his 'unfalsifying dream’. This is striking because quite often traditional elegies appear to present the opposite: a language which is ๐mate and images which are close to beatifying the deceased, putting them at a remove from human experience and existence. 'The Hawk in the Rain' is used to illustrate Hughes's theoretical position, especially in the case of his earlier war elegies and the circumstances of Remains of Elmet and Moortown Diary. He is both the observational, seemingly dispassionate poet (the hawk), capable of a detaching himself from the experience he wishes to relay in his verse, and yet, he is also the wanderer 'in the rain, one who is immersed in the momentous instant of his own language and experience. Like his personas, Hughes is divided. He is complicit with many of elegy's practices and traditions, but he is also a reformer and renovator of elegy, writing invigorating verse which brings the realities of mortality closer to the reader. In doing so, he reaffirms the significance of life and how this life might be better lived in closer harmony to poetry and contemporary ecological urgencies. 'The Elegies of Ted Hughes' aims to prove that far from being just a 'poet of nature', Hughes has been an exemplary elegist in our own time
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README_osu_daily_sla_geovel_v2.txt
No full textWe form a new data set of fields of sea level anomalies by combining gridded daily fields derived from altimeter data with coastal tide gauge data. Within approximately 50-80 km of the coast, the altimeter data are discarded and replaced by a linear interpolation between the tide gauge and remaining offshore altimeter data. A 20-year mean is subtracted from each time series (tide gauge or altimeter) before combining the data sets to form the merged sea level anomaly data set. Geostrophic velocity anomaly fields are formed from the surface heights. Daily mean fields are produced for the period 1 January 1993 - 31 December 2014. The primary validation compares geostrophic velocities calculated from the height fields and velocities measured at four moorings covering the north-south range of the new data set. The merged data set improves the alongshore (meridional) component of the currents, indicating an improvement in the data set
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osu_daily_sla_geovel_v3.md5
No full textWe form a new data set of fields of sea level anomalies by combining gridded daily fields derived from altimeter data with coastal tide gauge data. Within approximately 50-80 km of the coast, the altimeter data are discarded and replaced by a linear interpolation between the tide gauge and remaining offshore altimeter data. A 20-year mean is subtracted from each time series (tide gauge or altimeter) before combining the data sets to form the merged sea level anomaly data set. Geostrophic velocity anomaly fields are formed from the surface heights. Daily mean fields are produced for the period 1 January 1993 - 31 December 2016. The primary validation compares geostrophic velocities calculated from the height fields and velocities measured at four moorings covering the north-south range of the new data set. The merged data set improves the alongshore (meridional) component of the currents, indicating an improvement in the data set
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mean_aviso_field_1993_2012_v2.nc
No full textWe form a new data set of fields of sea level anomalies by combining gridded daily fields derived from altimeter data with coastal tide gauge data. Within approximately 50-80 km of the coast, the altimeter data are discarded and replaced by a linear interpolation between the tide gauge and remaining offshore altimeter data. A 20-year mean is subtracted from each time series (tide gauge or altimeter) before combining the data sets to form the merged sea level anomaly data set. Geostrophic velocity anomaly fields are formed from the surface heights. Daily mean fields are produced for the period 1 January 1993 - 31 December 2016. The primary validation compares geostrophic velocities calculated from the height fields and velocities measured at four moorings covering the north-south range of the new data set. The merged data set improves the alongshore (meridional) component of the currents, indicating an improvement in the data set
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osu_daily_sla_geovel_v2.md5
No full textWe form a new data set of fields of sea level anomalies by combining gridded daily fields derived from altimeter data with coastal tide gauge data. Within approximately 50-80 km of the coast, the altimeter data are discarded and replaced by a linear interpolation between the tide gauge and remaining offshore altimeter data. A 20-year mean is subtracted from each time series (tide gauge or altimeter) before combining the data sets to form the merged sea level anomaly data set. Geostrophic velocity anomaly fields are formed from the surface heights. Daily mean fields are produced for the period 1 January 1993 - 31 December 2014. The primary validation compares geostrophic velocities calculated from the height fields and velocities measured at four moorings covering the north-south range of the new data set. The merged data set improves the alongshore (meridional) component of the currents, indicating an improvement in the data set
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Blended sea level anomaly fields with enhanced coastal coverage along the U.S. West Coast. Version 3
No full textWe form a new data set of fields of sea level anomalies by combining gridded daily fields derived from altimeter data with coastal tide gauge data. Within approximately 50-80 km of the coast, the altimeter data are discarded and replaced by a linear interpolation between the tide gauge and remaining offshore altimeter data. A 20-year mean is subtracted from each time series (tide gauge or altimeter) before combining the data sets to form the merged sea level anomaly data set. Geostrophic velocity anomaly fields are formed from the surface heights. Daily mean fields are produced for the period 1 January 1993 - 31 December 2016. The primary validation compares geostrophic velocities calculated from the height fields and velocities measured at four moorings covering the north-south range of the new data set. The merged data set improves the alongshore (meridional) component of the currents, indicating an improvement in the data set
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osu_daily_sla_geovel_v2.tar
No full textWe form a new data set of fields of sea level anomalies by combining gridded daily fields derived from altimeter data with coastal tide gauge data. Within approximately 50-80 km of the coast, the altimeter data are discarded and replaced by a linear interpolation between the tide gauge and remaining offshore altimeter data. A 20-year mean is subtracted from each time series (tide gauge or altimeter) before combining the data sets to form the merged sea level anomaly data set. Geostrophic velocity anomaly fields are formed from the surface heights. Daily mean fields are produced for the period 1 January 1993 - 31 December 2014. The primary validation compares geostrophic velocities calculated from the height fields and velocities measured at four moorings covering the north-south range of the new data set. The merged data set improves the alongshore (meridional) component of the currents, indicating an improvement in the data set
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mean_aviso_field_1993_2012_v2.nc
No full textWe form a new data set of fields of sea level anomalies by combining gridded daily fields derived from altimeter data with coastal tide gauge data. Within approximately 50-80 km of the coast, the altimeter data are discarded and replaced by a linear interpolation between the tide gauge and remaining offshore altimeter data. A 20-year mean is subtracted from each time series (tide gauge or altimeter) before combining the data sets to form the merged sea level anomaly data set. Geostrophic velocity anomaly fields are formed from the surface heights. Daily mean fields are produced for the period 1 January 1993 - 31 December 2014. The primary validation compares geostrophic velocities calculated from the height fields and velocities measured at four moorings covering the north-south range of the new data set. The merged data set improves the alongshore (meridional) component of the currents, indicating an improvement in the data set
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README_osu_daily_sla_geovel_v3.txt
No full textWe form a new data set of fields of sea level anomalies by combining gridded daily fields derived from altimeter data with coastal tide gauge data. Within approximately 50-80 km of the coast, the altimeter data are discarded and replaced by a linear interpolation between the tide gauge and remaining offshore altimeter data. A 20-year mean is subtracted from each time series (tide gauge or altimeter) before combining the data sets to form the merged sea level anomaly data set. Geostrophic velocity anomaly fields are formed from the surface heights. Daily mean fields are produced for the period 1 January 1993 - 31 December 2016. The primary validation compares geostrophic velocities calculated from the height fields and velocities measured at four moorings covering the north-south range of the new data set. The merged data set improves the alongshore (meridional) component of the currents, indicating an improvement in the data set
Recommended from our members
Blended sea level anomaly fields with enhanced coastal coverage along the U.S. West Coast.
No full textWe form a new data set of fields of sea level anomalies by combining gridded daily fields derived from altimeter data with coastal tide gauge data. Within approximately 50-80 km of the coast, the altimeter data are discarded and replaced by a linear interpolation between the tide gauge and remaining offshore altimeter data. A 20-year mean is subtracted from each time series (tide gauge or altimeter) before combining the data sets to form the merged sea level anomaly data set. Geostrophic velocity anomaly fields are formed from the surface heights. Daily mean fields are produced for the period 1 January 1993 - 31 December 2014. The primary validation compares geostrophic velocities calculated from the height fields and velocities measured at four moorings covering the north-south range of the new data set. The merged data set improves the alongshore (meridional) component of the currents, indicating an improvement in the data set
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