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Coupling an atmospheric model to an ocean model to study air-ice-ocean interactions in Antarctica: challenges and applications

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(1)

Coupling an atmospheric model to an ocean model to study air-ice-ocean interactions in Antarctica:

challenges and applications

(2)

Introduction

High variability of ocean surface properties

 Parameters

 Sea Surface Temperature (SST)  Sea Ice

 Concentration, extent, thickness

 Temporal

 Seasonal (winter vs summer)  Annual

 Spatial

High variability of air-sea-ice interactions

(3)

Air-sea-ice interactions

Evaporation *

*

*

*

* Drifting snow Precipitations

(Snow + rain) Solar radiation

(4)

How to study the air-sea-ice system?

Atmosphere-Ocean General Circulation Model

(A-O GCM)

 To low resolution inadequate to study air-sea-ice interactions

Atmosphere-Ocean Regional Climate Model

(A-O RCM)

 High resolution and polar processes adapted

 But lateral boundaries conditions are required…

 In practice, Atmosphere RCM with prescribed sea surface

conditions

(5)

Prescribed sea surface conditions or “Swamp ocean”

 Less temporal variability of SSC

 For example, SSC are prescribed and constant during 6 hours  No feedbacks between atmosphere and ocean

Approximations in an atmosphere RCM

Warm Air Advection Sea Ice Sea Air Cooling Swamp ocean Warm Air Advection Sea Ice Sea Air Cooling Simplified reality

Melting at the sea ice surface

(6)

Physical challenges of a coupling

Differences of spatial and temporal scales between the

ocean and the atmosphere

 Ocean: smaller and slower  Atmosphere: larger and faster

Planetary waves Cyclones Cluster of Clouds Storms and Thunderstorms Convection and Cumulus Micro Turbulence Boundary layer Turbulence

(7)

Models have different resolutions (horizontal and

temporal) and different grids

 Interpolation

 Errors, especially near the coastline

 One of the two grid has to fully cover the other one  Combine data from forcing sets and coupled models

Technical challenges of a coupling

Global forcing data set

Ocean model grid

Atmosphere model grid Ice sheet

(8)

Conclusion and perspectives

Current models use major approximations

 Less reliable results

Coupling an ocean model to an atmospheric model

 Essential but physical and technical challenges

High resolution simulations of sea ice atmosphere

interaction

 Predictability of sea ice for operational purposes  Navigability for supply mission by ships for coastal bases  Modelling not/difficult measurable key parameters

 Assessment of blowing snow over sea-ice covered surface

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