A supervised neural network algorithm is used to categorize near‐global satellite retrievals
into three mesoscale cellular convective (MCC) cloud morphology patterns. At constant …

Diurnal warm layers develop in the upper ocean on sunny days with low surface wind
speeds. They rectify intraseasonal sea‐surface temperatures (SSTs), potentially impacting …

During the mid-Pliocene warm period (mPWP; 3.264–3.025 Ma), atmospheric CO 2
concentrations were approximately 400 ppm, and the Antarctic Ice Sheet was substantially …

Knowing future changes in the sea surface temperature (SST) is of vital importance since
they can affect marine ecosystems, especially in areas of high productivity such as the …

The assessment of expected changes in coastal sea surface temperature (SST) on a global
scale is becoming increasingly important due to the growing pressure on coastal …

The diurnal warm layer in the upper ocean develops during low surface winds and high
incoming solar radiation conditions, often increasing sea‐surface temperatures (SSTs) by up …

This study investigates the temporal and spatial complexities of the mean diurnal cycle (DC)
of precipitation over the Maritime Continent during the wet season using the Integrated Multi …

This study investigates the variations in air–sea heat fluxes and temperatures in two ocean
front regions, the Southwestern Atlantic Ocean (SWA) and the Drake Passage, widely …

Coupled climate models suffer from significant sea surface temperature (SST) biases in the
tropical Indian Ocean (TIO), leading to errors in global climate predictions. In this study, we …

A realistic representation of the Southern Ocean (SO) in climate models is critical for reliable
global climate projections. However, many models are still facing severe biases in this …