In its 24-hour outlook, the Meteorological Department of Oman said: "Mainly clear skies over most of the Sultanate with chances of cloud development over Al Hajar Mountains towards Wednesday afternoon and chances of cloudsadvection over Dhofar governorate." The sea will be moderate along the Arabian sea coasts with maximum wave height of 2 metres and along Oman coasts with maximum wave height of 1.5 metres.

Upper-air maps representing 850, 500, and 300 hPa included instructions to annotate troughs and ridges, shade areas of cold and warm airadvection (CAA/ WAA), positive (cyclonic) and negative (anticyclonic) vorticityadvection (PVA/NVA), and divergence and convergence.

The Directorate General of Meteorology in its forecast for May 16 and 17 stated that clear skies were expected over most of the sultanate withadvection of high and medium clouds.

Moreover, their implementation used a Semi-Lagrangianadvection model.

The atmosphere is relatively stable here, but this can be a good setup for bands of moderate to heavy snow and sleet, which meteorologists sometimes identify as being caused by something called "slantwise convection." It's far too technical to describe here, but we occasionally see it within warmadvection patterns where there is strong forcing.

The phenomenon on Friday wasadvection fog, when hot air from the land hits cooler air over the sea.

Advection fog occurs when hot air and cooler air mix, causing the cold air to cool rapidly while condensing into a thick wall of fog

hours, with continuous cloudsadvection and isolated rain while the

After explaining its basic properties, they describe its use in explicit Runte-Kutta methods, linear multi-step and predictor-corrector methods, some implicit methods, splitting techniques,advection problems, and other problems.

Visual foresight is based on 'convolutional recurrent video prediction,' or dynamic neuraladvection (DNA).

Over North America during winter and spring, the most frequent northerlyadvection (occurring on about one-fifth of days) was underestimated in all three model integrations, in which the frequency of the northern circulation type varied between 15% and 17% (Figure 6(a)).

In [4, 5], theadvection and diffusion terms are solved by two different numerical methods.