Moar freak weather in SoCal. Massive spray operations on top of unnatural tropical moisture sucked up from Baja (weather engineering) designed to make monsoons in a Dry Summer Subtropical Climate (Mediterranean) and “extreme weather” resulting in flooding in the mountains and desert for the fake news to exploit for normies glued to the media.
Here come the monsoons…. starting up with high winds over SoCal. Just a normal part of the season over a Mediterranean Climate they say? The normal climate of SoCal has been altered. Gone are the dry summers and westerly prevailing winds in the winter.
They spray the crap out of these (unnatural) tropical air masses which they can steer and stall at will, and saturate with nanotechnology “cloud seeding” that nobody talks about even when the spray is obvious to the naked eye.
https://www.weatherbug.com/news/Monsoonal-Rain-Brings-Flooding-Concerns-to-the-Wes?source=weather-forecast/now
The North American monsoon will be in full swing this week, drenching the Mountain West with plenty of rain and bringing concerns for flooding.
https://geo.libretexts.org/Bookshelves/Geography_(Physical)/The_Physical_Environment_(Ritter)/09%3A_Climate_Systems/9.05%3A_Midlatitude_and_Subtropical_Climates/9.5.01%3A_Mediterranean_or_Dry_Summer_Subtropical_Climate
9.5.1: Mediterranean or Dry Summer Subtropical Climate
The Dry Summer Subtropical climate, is also known as the "Mediterranean" climate because the land that borders the Mediterranean Sea is a type locality for this climate. The wet winter/dry summer seasonality of precipitation is the defining characteristic of this climate. Summer drought places a great deal of stress on the local vegetation, but plant structures have evolved to adapt to it. The small, thick evergreen leaves of the schlerophyll forest combat water loss during the drought conditions of the dry summer.
Controlling Factors
The main controlling factor over the characteristics of the dry summer subtropical climate is the alternating influence of the subtropical high in summer and Westerlies during the winter. During the summer, the subtropical high has expanded to its largest extent and most poleward position, exerting its influence on subtropical west coasts between 30o and 40o N and S latitude. Subsiding air from the high creates stable atmospheric conditions when coupled with cold ocean currents along these coasts. During the summer, stable maritime tropical air masses and cT air masses dominate.
During the winter the subtropical high shifts to the south and its influence is replaced by the Westerlies associated with the subpolar low. During this period, mT, mP, and cP air masses invade the climate. Midlatitude cyclones formed in the Westerlies bring much needed precipitation during the winter.
Precipitation
The most distinguishing characteristic of the dry summer subtropical climate is its seasonal precipitation regime. As discussed above, the dry summer is due to the presence of the subtropical high. The subsidence of the subtropical high suppresses cloud development and precipitation. Additionally, the presence of a cold ocean current along the western coast of the United States helps to stabilize the air, further reducing the chances for rain. The cloudless skies during summer, however, increase the absorption of insolation by the polluted atmosphere of many large urban centers in places like southern California causing problems of photochemical smog.
During the winter, the subtropical high shrinks and moves away from the climate and the subpolar low with its associated cyclone belts moves in. Uplift provided by cyclonic circulation brings much needed rain to this region. However, intense down pours can cause rapid runoff and initiate landslides on unstable slopes.
Total spray blot.
Manufactured monsoons over a Mediterranean climate? It’s just another day in clown world.