The subtidal behaviour of the Celtic Sea—I. Sea level and bottom pressures

Trends in UK mean sea level revisited

“…Linear regression yields regression coefficients of 9.9 ± 2.1 and 15.3 ± 2.6 mm mbar −1 , respectively, suggesting larger departures from the 'inverse barometer' (IB) at lower frequencies, as observed at many locations in the UK, Europe and elsewhere (e.g. Pugh & Thompson 1986;Mathers & Woodworth 2001). The departures will arise from forcings (e.g.…”

Trends in UK mean sea level revisited

“…Linear regression yields regression coefficients of 9.9 ± 2.1 and 15.3 ± 2.6 mm mbar −1 , respectively, suggesting larger departures from the 'inverse barometer' (IB) at lower frequencies, as observed at many locations in the UK, Europe and elsewhere (e.g. Pugh & Thompson 1986;Mathers & Woodworth 2001). The departures will arise from forcings (e.g.…”

Stable isotopic analyses of modern benthic foraminifera from seasonally stratified shelf seas: disequilibria and the 'seasonal effect'

“…(Pugh and Thompson, 1986). The study area is restricted to part of the northern Celtic Sea between 51°and 52°25'N between 4°and 7`W ( Figure 1).…”

“…The Celtic Sea extends from the 200 m isobath in the south and west of the continental shelf bordering the North Atlantic, to southern Ireland and the entrances to the Irish, Bristol and English Channels (Pugh and Thompson, 1986). The study area is restricted to part of the northern Celtic Sea between 51°and 52°25'N between 4°and 7`W (Figure 1).…”

10.1016/0967-0653(96)89885-1

“…Exchange of energy between the atmosphere and the ocean occurs at ail space and time scales and the resulting changes range from the sub-tidal to longer and secular motions. Chao and Pietrafesa (1980), Marmorino (1983), Pugh and Thompson (1986) and Lascaratos and Gacic ( 1990) discuss the subtidal and low-frequency response of the sea to different types of forcing, whereas Thompson (1980), Palumb and Mazzarella (1982), Spillane et al ( 1987) and Isoda et al ( 1991) study the longer and secular variability. The response of the semi-enclosed seas to the weather forcing is far from uniform.…”

Trends in UK mean sea level revisited

“…Linear regression yields regression coefficients of 9.9 ± 2.1 and 15.3 ± 2.6 mm mbar −1 , respectively, suggesting larger departures from the 'inverse barometer' (IB) at lower frequencies, as observed at many locations in the UK, Europe and elsewhere (e.g. Pugh & Thompson 1986;Mathers & Woodworth 2001). The departures will arise from forcings (e.g.…”

Stable isotopic analyses of modern benthic foraminifera from seasonally stratified shelf seas: disequilibria and the 'seasonal effect'

“…(Pugh and Thompson, 1986). The study area is restricted to part of the northern Celtic Sea between 51°and 52°25'N between 4°and 7`W ( Figure 1).…”

“…The Celtic Sea extends from the 200 m isobath in the south and west of the continental shelf bordering the North Atlantic, to southern Ireland and the entrances to the Irish, Bristol and English Channels (Pugh and Thompson, 1986). The study area is restricted to part of the northern Celtic Sea between 51°and 52°25'N between 4°and 7`W (Figure 1).…”

10.1016/0967-0653(96)89885-1

“…Exchange of energy between the atmosphere and the ocean occurs at ail space and time scales and the resulting changes range from the sub-tidal to longer and secular motions. Chao and Pietrafesa (1980), Marmorino (1983), Pugh and Thompson (1986) and Lascaratos and Gacic ( 1990) discuss the subtidal and low-frequency response of the sea to different types of forcing, whereas Thompson (1980), Palumb and Mazzarella (1982), Spillane et al ( 1987) and Isoda et al ( 1991) study the longer and secular variability. The response of the semi-enclosed seas to the weather forcing is far from uniform.…”

Trends in UK mean sea level revisited

“…Linear regression yields regression coefficients of 9.9 ± 2.1 and 15.3 ± 2.6 mm mbar −1 , respectively, suggesting larger departures from the 'inverse barometer' (IB) at lower frequencies, as observed at many locations in the UK, Europe and elsewhere (e.g. Pugh & Thompson 1986;Mathers & Woodworth 2001). The departures will arise from forcings (e.g.…”

Stable isotopic analyses of modern benthic foraminifera from seasonally stratified shelf seas: disequilibria and the 'seasonal effect'

“…(Pugh and Thompson, 1986). The study area is restricted to part of the northern Celtic Sea between 51°and 52°25'N between 4°and 7`W ( Figure 1).…”

“…The Celtic Sea extends from the 200 m isobath in the south and west of the continental shelf bordering the North Atlantic, to southern Ireland and the entrances to the Irish, Bristol and English Channels (Pugh and Thompson, 1986). The study area is restricted to part of the northern Celtic Sea between 51°and 52°25'N between 4°and 7`W (Figure 1).…”

10.1016/0967-0653(96)89885-1

“…Exchange of energy between the atmosphere and the ocean occurs at ail space and time scales and the resulting changes range from the sub-tidal to longer and secular motions. Chao and Pietrafesa (1980), Marmorino (1983), Pugh and Thompson (1986) and Lascaratos and Gacic ( 1990) discuss the subtidal and low-frequency response of the sea to different types of forcing, whereas Thompson (1980), Palumb and Mazzarella (1982), Spillane et al ( 1987) and Isoda et al ( 1991) study the longer and secular variability. The response of the semi-enclosed seas to the weather forcing is far from uniform.…”