It’s 92º and 9% humidity right now. I’m sitting with the door open and no cooling on and am perfectly comfortable. There is a ceiling fan turning slowly — and a breeze as there’s a thunderstorm in the mountains nearby, though not near enough to send the humidity up.
I love New Mexico.
The monsoon season hasn’t started yet though. The dew point is still in the 40s or lower. It needs to average 55 for three consecutive days before it’s deemed monsoon season. (The federales have decided the monsoon season is always to be June 15 – September 30 no matter the weather. But they think Washington’s Birthday is the third Monday in February too, so who cares what they say.)
Monsoon comes from the Arabic term for season or wind shift.
Both the Southwest USA, including Arizona and New Mexico, and Southeast Asia, including India, Pakistan, and Bangladesh, experience the monsoon each summer. The Asian monsoon often brings heavy, flooding rains to the area, while the Southwest monsoon brings scattered strong thunderstorms to dry desert regions. The Southwest monsoon is caused by two meteorological changes during the summer:
–The northerly movement of the Bermuda High (a strong area of high pressure) into the central USA
–Intense heating of the Mohave Desert to the west, which creates low pressure over the area
Since air rotates counterclockwise around low pressure and clockwise around high pressure, the positioning of these systems allows for a strong southerly flow over the Southwest. (Prevailing winds in the winter are from the west and northwest …) These south winds bring in moist air from the Gulf of Mexico and Pacific Ocean, increasing the chance of rain and thunderstorms.
The Weather Guys – USATODAY.com
Diagram is from August 2006, but it shows clearly how the monsoon draws humid air up from the Pacific and Gulf of Mexico. Click the image for larger version.
Update: In the spirit of full disclosure, the breeze stopped and I turned the cooler on.