Santander 2011 Monitoring the Rockall Trough Toby Sherwin 1 Penny Holiday 2, Jane Read 2, Clare Johnson 1 and many others, including Bill Turrell 3 (with.

Slides:



Advertisements
Similar presentations
OceanSITES by Svein Østerhus Station M (66N, 2E) Norwegian Sea North Atlantic Nordic Seas Exchanges Weddell.
Advertisements

Mooring Activities at SAMS NERC 4 th Moorings Workshop 15 th /16 th May 2008 Mooring Activities at SAMS NERC 4 th Moorings Workshop 15 th /16 th May 2008.
1 ICES/NAFO Symposium Santander May Seasonal to interannual variability of temperature and salinity in the Nordic Seas: heat and freshwater budgets.
RAPID/MOCHA/WBTS THE SEASONAL CYCLE OF THE AMOC AT 26ºN Eastern Boundary Considerations Gerard McCarthy, Eleanor Frajka- Williams, Aurélie Duchez and David.
Cutting edge Science and Research from a Glider Base in the North Atlantic by Toby Sherwin, Mark Inall, Estelle Dumont and Dima Aleynik Scottish Association.
Transports between Iceland and Scotland: Results from the Extended Ellett Line Clare Johnson (1), Stuart Cunningham (1), N. Penny Holliday.
G. Nolan 1, K.Lyons 1, S.Fennell 1, T. Mc Grath 1, D.Guihen 2, C.Cusack 1, C. Lynam 3 G. Nolan 1, K.Lyons 1, S.Fennell 1, T. Mc Grath 1, D.Guihen 2, C.Cusack.
PDO/PNA The PDO (Pacific Decadal Oscillation) is an index derived from North Pacific sea surface temperature anomalies and it has a high correlation to.
Seventh Meeting February Intense Attribution Period (IAP) 15 November April 2007.
The Faroe Current: T-S properties and volume, heat and salt transports Karin Margretha H. Larsen Bogi Hansen, Hjálmar Hátún, Svein Østerhus Extended Ellett.
3. Climate Change 3.1 Observations 3.2 Theory of Climate Change 3.3 Climate Change Prediction 3.4 The IPCC Process.
Wind driven seasonal variations in the transport of NAW through the Faroe-Shetland Channel also acknowledge: European Commission (MOEN – ASOF EU-E, Framework.
Climate Variability and Prediction in the Little Colorado River Basin Matt Switanek 1 1 Department of Hydrology and Water Resources University of Arizona.
News 8 Girl Scout Day November 1, 2008 “The El Nino Phenomenon” News 8 Austin Weather Burton Fitzsimmons.
NADW AABW AAIW Itay Halevy
RECENT OBSERVATIONS FROM THE 26ºN RAPID MOORING ARRAY: DROPS, DECLINES AND IMPACTS Gerard McCarthy National Oceanography Centre UK Molly Baringer, Adam.
Thermohaline Overtuning – at Risk? Detlef Quadfasel, THOR Project Office KlimaCampus, University of Hamburg, Germany
What weather phenomena has the largest impact on our weather in Texas?
Measurements in the Ocean Peter Challenor University of Exeter and National Oceanography Centre.
Thermohaline Circulation
Radiatively Active Gases from the N. Atlantic Region and Climate Change (RAGNARoCC) Andy Watson, UEA Biogeochemical sections for carbon and CFCs in the.
Two research cruises were successfully conducted in 2013 and Shipboard and moored observations show that: at first glance no significant decadal.
The North Atlantic Ocean and Climate Observing System Stuart A. Cunningham Scottish Association for Marine Science Barbara.
The role of gliders in sustained observations of the ocean Deliverable 4.1 or WP 4.
Tiree Passage (1981 – 2006) and Ellett Line Shelf Stations (1975 – 2005): Tides, Seasonality and Climatology Mark Inall, Phil Gillibrand, Colin Griffiths.
The La Niña Influence on Central Alabama Rainfall Patterns.
Indirect estimate of fluxes between boundary current and deep basins in the Nordic Seas: heat and freshwater budgets Katrin Latarius 1 and Detlef Quadfasel.
Steffen M. Olsen, DMI, Copenhagen DK Center for Ocean and Ice Interpretation of simulated exchange across the Iceland Faroe Ridge in a global.
Is the Transport of Atlantic Water in the Faroe Shetland Channel changing? – A summary of 20 years of observations Bee Berx1, Bogi Hansen2, Svein Østerhus3,
Dan Cayan Scripps Institution of Oceanography, UC San Diego USGS Water Resources Discipline much support from David Pierce, Mary Tyree, and other colleagues.
Ocean Weather Station M - from weather forecast to climate monitoring Ingunn Skjelvan Bjerknes Centre for Climate Research and Geophysical Institute, University.
DFO Northwest Atlantic Ocean Monitoring & Mooring Programs OSNAP Planning Meeting April 2011 BIO.
NACLIM CT 2 Monitoring of North Atlantic parameters Core Theme sessions Trieste 2 nd Oct 9:00-13:00 Lead: Svein Østerhus and Johannes Karstensen WP 2.1.
North Atlantic Observing System
THOR CT3 Meeting – Torshavn 2009 – Fischer/Visbeck/Zantopp/Nunes In the Labrador Sea, overflow water from the Denmark Strait and from the Iceland-Scotland.
MOC related activities at NOC Joël Hirschi, Elaine McDonagh, Brian King, Gerard McCarthy Stuart Cunningham, Harry Bryden, Adam Blaker SAMOC workshop, Rio.
AGU, 2003 image:AGU 2003 How will the Northeast Atlantic and its living resources respond to global climate change? Nordic Seas Greenland Iceland Norway.
Physical Oceanography Unit II. Physical Oceanography Physical oceanography is the study of the properties of seawater. There are 4 main topics: 1.Temperature.
Water Mass Distribution OEAS 604 Lecture Outline 1)Thermohaline Circulation 2)Spreading pathways in ocean basins 3)T-S diagrams 4)Mixing on T-S diagrams.
Evaluation of the Real-Time Ocean Forecast System in Florida Atlantic Coastal Waters June 3 to 8, 2007 Matthew D. Grossi Department of Marine & Environmental.
Seawater Chapter 15 Section 2.
Image:AGU 2003 Steingrímur Jónsson, University of Akureyri & Marine Research Institute Héðinn Valdimarsson, Marine Research Institute, Reykjavik Bogi Hansen,
Nutrient fluxes in the eastern North Atlantic Clare Johnson (1), Stuart Cunningham (1), Penny Holliday (2) and Stefan Gary.
Contributions from: Norwegian Meteorological Institute(met.no) Norwegian Meteorological Institute(met.no) Geophysical Institute, University of Bergen(GfI-UiB)
Lecture 9: Air-Sea Interactions EarthsClimate_Web_Chapter.pdfEarthsClimate_Web_Chapter.pdf, p ; Ch. 16, p ; Ch. 17, p
IPCC AR4 Chapter 5 Oxygen decline at base of pycnocline throughout subpolar and subtropical N. Pacific: reduced ventilation Deutsch et al. (2005) IPCC.
Michael J. McPhaden & Dongxiao Zhang NOAA/PMEL Decadal Variability and Trends of the Pacific Shallow Meridional Overturning Circulation and Their Relation.
Bogi Hansen & Hjálmar Hátún Faroe Marine Research Institute Iceland Scot- land Nordic Seas Faroes 0.8 Sv 3.8 Sv Greenland Østerhus et al., GRL 2005 The.
Page 1© Crown copyright 2004 The Uses of Marine Surface Data in Climate Research David Parker, Hadley Centre, Met Office MARCDAT-2, Met Office, Exeter,
Recent Variability in Ocean Climate in the Scotia-Maine and Adjacent Regions Brian Petrie, Roger Pettipas, Charles Hannah Bedford Institute of Oceanography.
Effect of the Subpolar Gyre on the eastern North Atlantic Clare Johnson (SAMS)*, Mark Inall (SAMS), Toby Sherwin (SAMS) *
Bogi Hansen, Hjálmar Hátún, Regin Kristiansen, Steffen M. Olsen and Svein Østerhus Iceland Scot- land Nordic Seas Faroes 0.8 Sv 3.8 Sv Greenland Østerhus.
© University of Reading 2011www.reading.ac. uk Tracking Earth’s Energy since 2000 Richard Allan University of Reading/NCAS climate Collaborators: Norman.
Increased oceanic heat transport in the main Atlantic inflow branch to the Nordic Seas Bogi Hansen, Karin Margretha H. Larsen Hjálmar Hátún,
Sampling the northern boundary of the North Atlantic:Cruise 159 of RRS Charles Darwin for RAPID Nick McCave and the crew of CD159*, Dept of Earth Sciences,
El Niño–Southern Oscillation (ENSO): What is it?
Spatial Modes of Salinity and Temperature Comparison with PDO index
from space Heat by winds by ocean currents
North Atlantic Sub-Polar Gyre
Ms. Halbohm Marine Biology
Ms. Halbohm Marine Biology
What weather phenomena has the largest impact on our weather in Texas?
David Tedesco Physical Oceanography
Processes and flow over the Iceland-Faroe Ridge
Ocean Circulation based on Density: Temperature and Salinity
The coupling between Atlantic inflow and overflow in the Iceland-Scotland region Bogi Hansen, Karin M. H. Larsen, Hjálmar Hátún, Svein Østerhus, Steffen.
Mid Atlantic Water Property Measurements W. S
RECENT DECLINE IN TYPHOON ACTIVITY IN THE SOUTH CHINA SEA
by M. A. Srokosz, and H. L. Bryden
Estimating ocean-shelf flux and exchange with drifters
Presentation transcript:

Santander 2011 Monitoring the Rockall Trough Toby Sherwin 1 Penny Holiday 2, Jane Read 2, Clare Johnson 1 and many others, including Bill Turrell 3 (with posthumous acknowledgement to David Ellett 1 ) 1 Scottish Association for Marine Science, Oban 2 National Oceanography Centre, Southampton 3 Marine Scotland, Aberdeen

AABW & LSW 0.9 Sv (0.3) NAW 0.6 Sv ~3 Sv Anton Dohrn The Rockall Trough Temperature / o C AABW ENAW LSW WTOW Salinity Anton Dohrn Rockall ENAW – Eastern North Atlantic Water WTOW – Wyville Thomson Ridge Overflow Water LSW – Labrador Sea Water AABW – Antarctic Bottom Water

Santander 2011 Three parts to talk: 1.Historical observation record 2.Future advances 3.Nutrients

Santander 2011 Three parts to talk: 1.Historical observation record 2.Future advances 3.Nutrients

Santander 2011 The Ellett Line Shared by SAMS and NOCS Regular sections since 1975 Initially 4 times a year More recently annually Nutrients since 1996 RRS Challenger David Ellett

Santander 2011 θ and S across the Rockall Trough Annual std dev indicated Averaged three times i)Across the RT ii)Between 30 and 800 m iii)By year (when >1 cruises) θ increase reversal S increase levelling out

Santander 2011 Labrador Sea Water east of Anton Dorhn For a definition of LSW see the IROC θ and S at ~ 1750 m

Santander 2011 Observations by Ocean Weather Ships UK Met Office 1948 to 1992 Various tracks S of Anton Dorhn Surface T and S Measurement technique changed over time Averaged across the trough by Ellett and Jones, MAFF Rpt 36, 1994 Look at winter months JFM

Santander 2011 OWS Surface θ and S across RT Great salinity anomaly JFM averages Annual averages

Santander 2011 OWS Surface Temperature and Salinity across RT Towed thermometer Mercury in board Autolab salinometer Guildline salinometer Thermistors In board sampling Titration

Santander 2011 Synthesis of Sea Surface Temperatures HadiSST - UK Met Office 1856 onward by vessels of opportunity Synthesis of sea surface temperature (SST) only Area average into 5 o by 5 o boxes

Santander 2011 HadiSST JFM averages HadiSST SSTs in the north-eastern North Atlantic

Santander 2011 Surface versus deep observations Ellett Line + top 4 m ● 30 to 800 m ?

Santander 2011 Part 1 conclusions: 1.OWS surface salinity seem good before HadiSST SSTs seem to be ‘reasonable’ proxy for RT winter water column temperatures The standard Ellett Line data are the ‘gold standard’ But will that always be the case?

Santander 2011 Three parts to talk: 1.Historical observation record 2.Future advances 3.Nutrients

Santander 2011 Argo tracks in the RT to March 2011

Santander 2011 Glider observations Operated SAMS Started winter 2009/2010 Continuous monitoring to 1000 m Latest mission started May 2011

Santander 2011 Glider temperature and salinity winter 09/10

Santander 2011

Gliders are adding to the annual cruise data

Santander 2011 Three parts to talk: 1.Historical observation record 2.Future advances 3.Nutrients

P314 July 2004 NO23 (μM) PO4 (μM) Si (μM) Rockall A ‘typical’ year July 2004

Temperature / o C AABW ENAW LSW WTOW Nutrient profiles East of Anton Dorhn NO23 PO4 Si West of Anton Dorhn NO23 PO4 Si

Nutrient time series east of Anton Dohrn Month of cruise indicated

D321 Nutrient time series west of Anton Dohrn Month of cruise indicated

Santander 2011 Nutrient observations since 1996

Santander 2011 Conclusions (wrt last decade) The rise in surface temperature since 1995 seems to be tailing off Salinities continue to rise and have returned to pre-GSA levels Neither θ nor S levels appear significantly higher than historical values, but … LSW signature continues to freshen and cool There are real trends in nutrient levels need to be explained by a nutrient chemist

Santander 2011 Chnbo Guo Svein Osterhus Detlef Quadfasel Bogi Hansen