It is a natural question for a Northwesterner.   What time of  the day is wettest and driest on average?  When should you schedule that  walk or hike, early or late in the day?
In most places  there IS a time when precipitation is most likely, but in some  locations the diurnal (daily) modulation is weak.   The daily  precipitation cycle not only varies geographically, but also seasonally.
So what causes rainfall to vary around the day?  Some reasons:
1.   As air cools at night, the relative humidity  tends to rise, leading to more drizzly fog and stratus during the  morning hours with a peak near or just after sunrise.
2.   As the surface heats during the summer the temperature variation with  height (the lapse rate) increases, leading to more convection  (thunderstorms and convective showers) during the afternoon.
3.   Sea breezes develop during the morning and push inland around  lunchtime.  Showers can occur at the leading edge of the cool marine  air:  the sea breeze front.
In general, diurnal variation of precipitation is largest during  the summer months, when the sun's heating is strongest and thunderstorms  are most frequent.
Well,  what about western Washington?  I did a  paper on diurnal weather variations around here and below is a graph  showing the typical mid-summer diurnal variation in sky cover and  precipitation.  Both tend to be most frequent around 3-8 AM.  This makes  a lot of sense.  We don't get many thunderstorms around here and low  clouds and drizzle sometimes occur when the region is flooded by marine  air.  Often the clouds burn off or lift by late morning.  So plan your outdoor activities in the afternoon or early evening!   But take a look at the actual numbers...the variation is only from 4 to  5.5 % chance of rain during any three-hour period.   Not a strong  signal.
If  you want a bigger signal you need to look eastward to places that have  thunderstorms.  Here is a neat figure produced by some folks at NASA  showing summertime (July-August)  precipitation timing across the U.S.   The first figure shows the amplitude of the daily precipitation  variations:  over the for western U.S., where there is little summer  convection, the diurnal amplitude is very small....just the morning  drizzle.   You want a big daily variation head for Florida--the  thunderstorm capital of the U.S.!
The second figure  tells you the time when precipitation is most frequent in Local Standard  Time. For the Rockies, Southeast and Eastern U.S., precipitation is  most frequent between noon and 6 PM (greens to yellows), but over the  Great Plains, there is an evening and early morning maximum.  Why?  It  turns out that a lot of convection builds over the Rockies and  progressively moves out into the {lains over time.  There is also an  influence of a low-level jet that I won't get into here.
 The  last figure shows the time of minimum precipitation; for the Rockies  the the eastern U.S., it is overnight...and during mid-day over the High  Plains.
During the winter the precipitation variations are much less.   There is no color graphic that I know of, but Mike Wallace of my  department prepared the next figure.  The
amplitude of the daily  precipitation variation is indicated using wind barbs...just like the  wind plots I have shown you.  More barbs, the stronger the cycle.  Not  very strong anywhere.  The time of maximum precipitation is shown by the  direction of the barbs.  Pointing from the east:  6 AM max.  Point from  the south:  noon max., etc.  Thus the Northwest max precipitation  mainly occurs between 6 AM to noon.  Much of the rest of the country  around 6 AM.   Thus, it appears that early morning is the WORST time to  be up and about if you want to avoid rain during the cool season.  Any teenager or college student can tell you that those are times to avoid. 
Portland Talk:   Just a heads up...I will be giving a talk on the Future of Northwest Weather Prediction in Portland on Saturday, May 12th at 10 AM.   Location:  OMSI--the Portland Science Museum.  There is no charge to attend (sponsored by the Portland Chapter of the American Meteorological Society).  For more information check here.


No comments:
Post a Comment