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Physical Properties and Forcings in an Estuarine System 2013 PICES Summer School Group 4 Matthew, Daniel, Jingsong, Chorong, Joocheul, Morgaine, Polina,

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Presentation on theme: "Physical Properties and Forcings in an Estuarine System 2013 PICES Summer School Group 4 Matthew, Daniel, Jingsong, Chorong, Joocheul, Morgaine, Polina,"— Presentation transcript:

1 Physical Properties and Forcings in an Estuarine System 2013 PICES Summer School Group 4 Matthew, Daniel, Jingsong, Chorong, Joocheul, Morgaine, Polina, Amy

2 Topic: Physical Oceanography Question: Describe the time dependence in physical properties (temperature, salinity, dissolved oxygen) and explain what forces these.

3 Yaquina Bay: 2 Sites, 1.5 Days Mooring w/ CTD CTD casts

4 Mooring

5 Winds – upwelling favorable

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8 Y14 Sample Times (m) Aug. 20Aug. 21 Δh = 5cm Δh = 46cm

9 Y14

10 Trends Day 1: Day 1: –well-mixed throughout Day 2: Day 2: –well-mixed below 3m –lower T, higher S, lower DO (rel. to day 1) No apparent tidal influence in CTD cast data at Y14 station No apparent tidal influence in CTD cast data at Y14 station –sampling on opposite sides of tidal peak (not at extremes) –Day 2: 2 nd sample in the slack tide

11 Hypotheses 1: Well-mixed water column due to low summertime river flow relative to tide flow. 1: Well-mixed water column due to low summertime river flow relative to tide flow. 2: Day 2 had more upwelled ocean water at Y14. 2: Day 2 had more upwelled ocean water at Y14. –stronger tide, wind from the N –T decreased, S increased, DO decreased

12 Vertical velocity differences are small

13 Potential issues Non-verticality of cast Non-verticality of cast –drift of boat during sampling –strong currents  CTD line angled Non-shared datum Non-shared datum –depth relative to surface –up to 0.5m change in depth (flood vs. ebb)

14 Conclusions Upwelled water is identifiable at both stations on Day 2 Upwelled water is identifiable at both stations on Day 2 River water is not a strong influence: low flow rates  strong mixing  well-mixed water column (no salt wedge) River water is not a strong influence: low flow rates  strong mixing  well-mixed water column (no salt wedge) CTD sampling must be better spaced along tidal cycle to make conclusions about effects of the tide with only discrete sampling CTD sampling must be better spaced along tidal cycle to make conclusions about effects of the tide with only discrete sampling

15 Thank you GRACIAS!!!! GRACIAS!!!! GAMSAHAMNIDA!!!! GAMSAHAMNIDA!!!! ARIGATOU!!!! ARIGATOU!!!! DANKE SCHOEN!!!! DANKE SCHOEN!!!! CHEERS MATES!!! CHEERS MATES!!! SHYE SHYE! SHYE SHYE! SPACIBO!!! SPACIBO!!!

16 Backup Slides

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19 Day 1: Flood tide

20 Day 1: Ebb tide

21 Day 2: Flood tide

22 Day 2: Ebb tide

23 Tidal cycles in flow-through Temperature decrease & salinity increase as flood tide comes in Temperature decrease & salinity increase as flood tide comes in Temperature & salinity relatively constant for samples around max tide point Temperature & salinity relatively constant for samples around max tide point

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28 Group1

29 Group2

30 Group3

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