Download presentation
Presentation is loading. Please wait.
Published byShauna Reed Modified over 8 years ago
1
Tiree Passage (1981 – 2006) and Ellett Line Shelf Stations (1975 – 2005): Tides, Seasonality and Climatology Mark Inall, Phil Gillibrand, Colin Griffiths Neil MacDougal, Kimberly Blackwell, Graham Walkden
2
Outline Oceanographic context: NW UK Shelf The “Observatory” Tiree Passage “continuous” time series –Variability: tidal to inter-decadal –Forcing of residual flow Ellett Line shelf stations: shelf-wide context Where do we go from here?
3
Circulation Ellett and Edwards schematic circulation of the NW UK Shelf Based on a variety of sources, including 137Cs distributions
4
Surface Salinity
5
Semi-diurnal tides ( POLCOMS )
6
Moorings Met. Stations Tide gauges CTD Section SST/SSS Station (Port Erin) The “Observatory” plus satellite imagery, model products and ‘foul weather CTD opportunities’
7
AVHRR 11 May 2000. Peter Miller PML
8
POLCOMS
9
Ellett Line 75 occupations since 1975 SAMS 1975 – 1992 NOC 1992-1995 SAMS/NOC Joint 1996 - present No occupations in 1986 and 2002 SAMS Northern Seas Programme Occupations in 2001 (partial) 2003 (full), 2005 (partial), 2006 (happening now!) Tiree Passage: Longest temperature and flow time series on the NW European continental shelf June 1981: Hourly current and temperature (11 m a.b.) November 1987 2 nd meter added at 22 m a.b. Ended in September 1997 at both depths. Restarted June 1999 to February 2000 and then May 2002 until the present with RCMs at 11m and 22 m a.b. Seabird salinity added in August 2002 at 22 m above bed. A total of 61 deployments.
10
Raw Tiree time series Inevitable gaps, but tidal to inter-annual (decadal?) variability captured Temperature Velocity
11
Tiree Variability Temperature: SA dominant, weak tidal Along channel velocity: tides dominate, SA significant X-channel velocity: tides and broad SA dominate
12
Northward residual flow Residual flow for full time series = 10.8 cms -1 northwards Equating to 6.7 10 4 m 3 s -1 SA clear in monthly means
13
Moorings Met. Stations Tide gauges CTD Section SST/SSS Station (Port Erin) The “Observatory” plus satellite imagery, model products and ‘foul weather CTD opportunities’
14
Tiree Passage Barotropic dynamics Correlation Coefficients = 0.11 = 0.46 = 0.53 = 0.83 = 0.08 = 0.12 = 0.03 (local only)
15
Atmospheric forcing of residual flow: NAO Index r = 0.59
16
Tiree temperature anomalies Irish Sea vs. NE Atlantic TIME SERIESr2r2 SIGNIFICANT Tiree and Port Erin0.5047Yes Tiree and Rockall0.1674Yes Port Erin and Rockall0.1117Yes Tiree and Q net 0.0005No Port Erin and Q net 0.0423Yes Rockall and Q net 0.0071No
17
Port Erin vs. Tiree Passage
18
Coastal warming trend 0.57 C per decade. Note broad cooling in late 1980s and early 1990s, and peaked warm episodes of late 1980s and 1990s.
19
Seasonal shifts Advance of date of maximum temperature by 9 days/decade: clearly not sustainable. No significant trend in date of minimum temperature
20
Reliable salinity - only recently: seasonality? Probably not (Ellett Line) – too early to tell
21
Shelf-wide Context
22
Ellett Shelf Stations
23
Seasonally adjusted bottom and surface (10m) temperature.
24
Salinity Climatology Salinity trend –Surface (10m) +0.044 psu/decade –Bottom +0.036 psu/decade
25
Where do we go from here? Modeling context for –Process studies of cross shelf exchange –30 year Hindcasts of inter-annual variability X-shelf surface elevation data Acoustics Time to work on the data !
26
Predictive Capability ? Karemia mikimotoi bloom during summer 2005 Progression of bloom from Mull – Lewis – Orkney - Shetland MODIS Aqua image, 31 July 2005 (RSDAS)
Similar presentations
© 2024 SlidePlayer.com Inc.
All rights reserved.