Impact of an improved radiation scheme in the MAECHAM5 General Circulation Model

Here, we focus on the presentation of the “large scale features” of Pliocene climate, that is, global annual mean surface air temperature response (di ff erence from the

Conversely, the calculated harmonic mean temperature was 306.68 K, which is significantly different and higher than values of the reported isokinetic temperature, confirming

Right column: di ff erences of quantiles between mean observed and sim- ulated temperature anomalies with “dynamic” weather generator with a 21 December 2009 initialization...

While the realizable k- ε realizable model gives a reasonable prediction of temperature and velocity profiles in the de Villiers [12] study, the k- ω SST model employed in the

Eddy core anomalies from the di ff erence between profiles outside the eddy and in the eddy core (as shown in the section plots) versus depth for salinity, temperature, density

The top two panels show the normalized surface air temperature di ff erence between weak and strong AMOC states (as defined in Fig. 2) under Preindustrial and Glacial

calculated using di ff erent values of mean annual temperature as input for the PDD model, but to facilitate comparison with the SMB gradient method, the results are plot- ted as

Sensitivity of AIRS and IASI brightness temperature variances to wave perturbations with di ff erent vertical wavelengths (left) and horizontal wavelengths (right). Sensitivity