RAPID @ The University of Liverpool

Department of Earth and Ocean Sciences
Physical Oceanography group



RAPID Climate Change

1. Preliminary model experiments


Performed with North Atlantic coarse resolution isopycnal model (MICOM 1.7):
1.4 deg. horisontal resolution (Mercator grid), 6 sigma layers (26.0, 27.0, 27.5, 27.7, 27.8, 27.9). The model is forced by annual mean winds, initial conditions are taken from Levitus. Isopycnal interfaces are relaxed to Levitus in the northernmost part (61-65N). In oreder to preserve the mean vertical stratification implicit diapycnal mixing is introduced, which compensates for the dense water inflow from the northern boundary. Isopycnic diffusion/mixing parameters: biharmonic thickness diffusion; diffusion velocity 0.5 cm/s Laplacian tracer diffusion; diffusion velocity 0.5 cm/s, momentum mixing velocity 1 cm/s with deformation dependence.
The model is run for 110 years with deep northern tracer released during the last 10 years - this is the set-up for the standard or reference run. Twin experiment is run during the last 10 years, which is forced to produce extra deep water by gradual uplift of upper interfaces of layer 4 and 5 - 120m/10 days over the north relaxation region. After this perturbation, the interfaces are kept at the new positions.

Download movie (1.9Mb)

Layer thickness - tracer
Left pannel: perturbed layer thickness (shaded), deep transport (contours in Sv)
Right pannel: Labrador sea tracer after 10 years

Time series
Layer thickness (solid lines) ; Labrador Sea tracer (dashed lines)
Green - reference ; black - perturbed experiment

Hovmueller diagram
Difference in interface depths (pressure) of layer 27.85 (reference-perturbed)
Labrador tracer - contours

Download EGS2003 poster (0.4Mb)

2. High resolution model experiments


The model set-up is same as the coarse resolution model, but the horisontal resolution is increased to 0.28 deg. (~30km at the EQ, 15km at 60N). The model is run for 44 years with deep northern tracer released during the last 4 years - this is the set-up for the standard or reference run. Twin experiment is run during the last 4 years, similar to the coarse resolution experiments.

Download movie (1.7Mb)

Time series
Layer thickness: green - reference ; black - perturbed experiment ; red - Labrador Sea tracer

Hovmueller diagram
Difference in interface depths (pressure) of layer 27.75 (reference-perturbed)

Correlation patterns

Download 2004 PPT presentation (1.4Mb)
Download 2004 poster (PPT 1.3Mb)

Transport anomaly

Monthly mean wind forcing experiment: the model is run for 44 years, forced by ECMWF monthly mean fields. The thermohaline forcing is kept constant. Last four years have been subsampled every 5 days and diagnosed.
Download movie (2.9Mb)
Download 2005 PPT presentation (2.2Mb)

3. Recent experiments

The model set-up is similar, but the resolution is increased to 0.23 deg. in horisontal and 16 vertical layers. The model domain is extended: 35S - 67N.

Model topography
Kinetic energy
SSH
25W section
Anomaly propagation
Transport anomaly monthly forcing
Transport anomaly annual mean forcing
SSH/SST movie - monthly mean forcing
SSH/SST movie (5.6 MB QuickTime Movie)
SST movie - monthly mean forcing

Download EGS2006 poster
Download RAPID2006 poster
Download RAPID2007 poster
Download RAPID2008 poster
Download RAPID2010 poster
Download RAPID2011 poster


This page is under construction!! Maintained by V. Roussenov, vassilr@liv.ac.uk
Last changed 08 July 2011