A Three-Dimensional Heatwave
Yesterday (Friday, April 28) was the first moderately warm day of the Northwest "summer" season, with temperatures ranging from near 90F along the western slopes of the Cascades to around 70F near the water (see a map of high temps below) Why were the warmest temperatures along the western slopes of the Cascades? It turns out that the Friday heat was very three-dimensional. Water provided some cooling, but the situation was much, much more complex than that. We need to start with the sea-level pressure pattern, with the one at 11 AM Friday shown below. High pressure over eastern Washington and low pressure over northwest Oregon and southwest Washington resulted in an easterly (from the east) wind moving over the Cascades. But at low levels around Puget Sound winds were from the north, since pressures were higher over northwest WA and lower over western Oregon. Near mountains, winds like to go from high to low pressure. A schematic of the situation around Puget Sound