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Sea Ice. Big Questions: What are the quantitative contributions of various processes to ice mass balance over the annual cycle. What positive and negative.

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Presentation on theme: "Sea Ice. Big Questions: What are the quantitative contributions of various processes to ice mass balance over the annual cycle. What positive and negative."— Presentation transcript:

1 Sea Ice

2 Big Questions: What are the quantitative contributions of various processes to ice mass balance over the annual cycle. What positive and negative feedbacks may change significantly in a future Arctic. What are the linkages of sea ice changes with other systems, including ecosystems, mid latitudes, carbon cycling…

3 Big Questions: What are the quantitative contributions of various processes to ice mass balance over the annual cycle. What positive and negative feedbacks may change significantly in a future Arctic. What are the linkages of sea ice changes with other systems, including ecosystems, mid latitudes, carbon cycling… Similarity to SHEBA objectives noted

4 What was missing at SHEBA? What do modelers need? Measurements of Heterogeneity – Snow/Ice thickness distribution – Ice surface and bottom roughness – Snow redistribution – Internal melt – Under ice radiation field Observations of the “New Arctic” (open ocean – ice transition states) – Thin ice, upper ocean cooling. – Logistics challenges… must be met. SHEBA

5 What was missing at SHEBA? What do modelers need? Measurements of Heterogeneity – Snow/Ice thickness distribution – Ice surface and bottom roughness – Snow redistribution – Internal melt – Under ice radiation field Observations of the “New Arctic” (open ocean – ice transition states) – Thin ice, upper ocean cooling. – Logistics challenges… must be met. SHEBA LiDAR, Multibeam on ROV Airborne Radar and EM, RS assets, UAV’s LiDAR Micro CT Logging Spectroradiometers

6 What was missing at SHEBA? What do modelers need? Biological impacts – EPS – ice structure/strength interactions – Light Transmission (time series) – Porosity/permeability - nutrient cycling relations – DMS production/release – Bacterial/algae linkages Biogeochemical cycling – DIC pump to deep ocean – Brine movement Spatial/Temporal extensions – Cal/Val of Remote sensing – Autonomous platforms SHEBA

7 What was missing at SHEBA? What do modelers need? Biological impacts – EPS – ice structure/strength interactions – Light Transmission (time series) – Porosity/permeability - nutrient cycling relations – DMS production/release – Bacterial/algae linkages Biogeochemical cycling – DIC pump to deep ocean – Brine movement Spatial/Temporal extensions – Cal/Val of Remote sensing – Autonomous platforms SHEBA Molecular Techniques Logging Spectroradiometers, ROV’s Micro CT, Analytical techniques

8 Lots of cool stuff… Linkages – A way to prioritize

9 Ocean Summer heating/fall freezing Freshwater exchange Deepwater formation Sediment entrainment Coupling, both momentum transfer and mixing

10 Linkages – A way to prioritize Atmosphere Long/Shortwave Snow Surface Roughness/Turbulent Flux Biological Processes EPS – ice structure/strength interactions Light Transmission (time series) Porosity/permeability - nutrient cycling relations DMS production/release

11 Other Thoughts Observation vs. Experimentation Heisenberg's Uncertainty Principle Dance Card: Temporal Spatial SynopticSeasonal Decadal- Climate Local Regional Global

12 Big Questions: What are the quantitative contributions of various processes to ice mass balance over the annual cycle. What positive and negative feedbacks may change significantly in a future Arctic. What are the linkages of sea ice changes with other systems, including ecosystems, mid latitudes, carbon cycling…


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