'Surface salinity' presentation slideshows

Climate impacts on Puget Sound circulation and ecology

Climate impacts on Puget Sound circulation and ecology. Jan Newton University of Washington. PNW est uaries have strong influence from climate Global influence on: ocean conditions watershed conditions local weather. NASA SeaWiFS Image.

445 views • 32 slides

Lecture 2 - Major Ions in Sea Water

Lecture 2 - Major Ions in Sea Water. Why do we care about the major ions? What is the composition of seawater? What defines Major Ions? What are their concentrations? What are their properties?. Density: distributions and controls (salinity and temperature). Density of Seawater.

433 views • 28 slides

403 views • 27 slides

Surface Circulation Pathways

Surface Circulation Pathways. Generally, warm currents move poleward and cool currents move equatorward. Effect of Ocean Heat Transport. Pattern of currents flow impacts sea surface temperatures and, as a result, air temperatures over land. Equatorial Pacific: Sea Surface Temperature (SST).

454 views • 27 slides

Sea-Level Rise Impact on Salinity in the York and Chickahominy Rivers

Sea-Level Rise Impact on Salinity in the York and Chickahominy Rivers. Mark Bennett, USGS Study funded Cooperatively with Newport News Waterworks. Acknowledgements. Presentation derived primarily from study entitled:

370 views • 24 slides

SPURS Discussion Ray Schmitt/Eric Lindstrom Wed., July 21, 2010

SPURS Discussion Ray Schmitt/Eric Lindstrom Wed., July 21, 2010. Potential location for a process study. Objectives: What processes maintain the salinity maximum? Where does the excess salt go? What processes give rise to temporal variability?

344 views • 23 slides

Bridging the Gap between idealized and realistic numerical river plume simulations

Bridging the Gap between idealized and realistic numerical river plume simulations. Robert Hetland Texas A&M University. Feedback between idealized and realistic modeling. Numerical consistency. Metrics (Depends on user requirements). Idealized modeling. Realistic modeling.

353 views • 22 slides

Remotely Sensed Estimates of Surface Salinity and Environmental Vibrio in the Chesapeake Bay

Remotely Sensed Estimates of Surface Salinity and Environmental Vibrio in the Chesapeake Bay. Erin Urquhart 1 , Matt Hoffman 2 , Ben Zaitchik 1 , Seth Guikema 1 1 Johns Hopkins University, 2 Rochester Institute of Technology. Chesapeake Bay. Salinity gradient Oligohalic (0-6 ppt )

350 views • 22 slides

MOSAiC M ultidisciplinary drifting O bservatory for the S tudy of A rct i c C limate

324 views • 21 slides

Evidence for high-frequency (10 4 -10 5 yr) glacial-eustasy during Paleozoic greenhouse intervals

Evidence for high-frequency (10 4 -10 5 yr) glacial-eustasy during Paleozoic greenhouse intervals. Bethany P. Theiling a,b and Maya Elrick a a University of New Mexico b Purdue University . Purdue Stable Isotope (PSI) Facility.

315 views • 21 slides

Structure and Variability of Middle Atlantic Bight Hydrography

Structure and Variability of Middle Atlantic Bight Hydrography Charles Flagg and Alexandra Sanchez-Franks New York Marine Sciences Consortium Symposium September 22, 2012. The Oleander Project. Hudson River Plume in the New York Bight Apex

359 views • 20 slides

Distribution of waters

219 views • 15 slides

Effects of Salinity Variability in a low wind speed Environment in the BVW Model

Effects of Salinity Variability in a low wind speed Environment in the BVW Model. Danielle Niles & Steven Martinaitis Physics of the Air-Sea Boundary Layer OCP 5551 Dr. Mark Bourassa The Florida State University. Outline. Introduction Problem and Background Data & Methodology Results

360 views • 15 slides

NDBC Capabilities in the Northern Gulf of Mexico Hypoxic Zone Summit 30 January, 2007

NDBC Capabilities in the Northern Gulf of Mexico Hypoxic Zone Summit 30 January, 2007 Sept 2006. NOOSS. NDBC Ocean Observing System of Systems: Coastal (Yellow) Buoys CMAN Stations TAO Array DART Network Partner Data via IOOS DAC.

256 views • 14 slides

Overturning of the Antarctic Slope Front and glacial melting along the coast of Dronning Maud Land

228 views • 14 slides

In the mid-Pleistocene, the period of glacial cycles changed from 41kyr to 100kyr.

In the mid-Pleistocene, the period of glacial cycles changed from 41kyr to 100kyr. The zonal SST gradient increased during MPT due to the cooling in the EEP and relatively stable WEP. Correlation of interannual SST anomalies between the site of Hole 806B and other regions of the tropics.

210 views • 13 slides

GODAS Ocean Climate Modeling at NCEP

GODAS Ocean Climate Modeling at NCEP. David W. Behringer. Aquarius Workshop Silver Spring, MD November 29, 2011. The role of GODAS. Provide initial conditions for coupled SI climate forecasts Provide a means for monitoring the ocean climate. Climate Forecast System (CFSv1). CFSv2.

237 views • 11 slides

Thursday February 28, 2013

280 views • 11 slides

V.v.= ? 0 + ? 1 (Temp) + ? 2 (Saln) + ? 3 (Temp*Saln)

V.v.= ? 0 + ? 1 (Temp) + ? 2 (Saln) + ? 3 (Temp*Saln). Urquhart et al. (2012) Remotely Sensed Estimates of Surface Salinity in the Chesapeake Bay: A Statistical Approach. RSE. 123. V. parahaemolyticus 9/18/2006. V. vulnificus 9/18/2006.

166 views • 3 slides

Mechanisms of the North Atlantic multidecadal internal variability in the CNRM-CM5 model

Low-pass filtered AMOC Leading EOF (80%). Profondeur (m). 2Sv between Iso-contours. Eq. S. N. N. N. N. Sv. Mechanisms of the North Atlantic multidecadal internal variability in the CNRM-CM5 model Y. Ruprich-Robert ( ruprich@cerfacs.fr ) and C. Cassou ( cassou@cerfacs.fr ).

123 views • 1 slides