Implication of methodological uncertainties for Mid-Holocene sea surface temperature reconstructions

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

Some examples of these works in chronological order, are: [32] studied the relation between the Sea Surface Temperature (SST) pattern over the Atlantic and the Pacific Oceans and

The model simulates the main features of observed sea surface temperature (SST) pattern during the summer months showing the upwelling along the coastal boundary with

Because of the increas- ing the speed of the decomposition of the anhydrite, together with the growth of the temperature of casting the bronze to the plaster mould, the gases

We demonstrate, however, that changes in the sea surface temperature (SST) gradient and mid-latitude eddies are instrumental in creat- ing a similar deep vertical temperature

The Metop AVHRR Arctic Surface Temperature product (MAST) is an integrated IST, marginal ice zone temperature and high-latitude/Sea Surface Temperature product (SST), developed in

face air temperature anomalies obtained using the nudging; blue line: surface air temperature anomalies obtained using the sequential importance resampling; red line: surface

Here, we investigate the relationship between climatic parameters [rainfall, temperature, humidity, sea surface temperature (SST), El Nin˜o-Southern Oscillation (ENSO), the