A more detailed analysis of linear 2004–50 SAT trends as a
function of terrain elevation is given in Fig. 5. In the SMHI-RCAO and MetNo-HIRHAM runs,
SAT trends increase with height up to about 600 m. Above that elevation and to the
top of the
terrain, trends remain constant in the SMHI-RCAO, but decrease slightly in the MetNo-HIRHAM.
In the DMI-HIRHAM5, warming rates over the ocean and at low
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