During the last ten years, many regions in California have experienced record-breaking extremes that have included some of the wettest and driest years on record. The 2019-2020 rainy season marked another extraordinary chapter in the increasingly strange weather patterns that have puzzled and often plagued Californians in recent years. We will first lead you toward National Weather Service Lead Forecaster David Gomberg’s slides that summarized our state’s situation at the end of the season. We will follow with a series of images and maps that tell a more detailed story about our latest abnormal Golden State rainy season, 2019-2020. We occasionally separate these presentations with colorful scenes on the ground (from spring to late June) that show how the state’s ecosystems and landscapes responded to these odd weather patterns.
For now, we can learn from the images prepared by David Gomberg as the rainy season ended in May. David is Lead Forecaster/Fire Program Manager at the L.A./Oxnard National Weather Service office and he shared his work during a workshop organized for college educators by Senior Meteorologist Todd Hall, with contributions from other meteorologists there. We are reminded again that all U.S. weather information and forecasts originate from the National Weather Service. These dedicated scientists use their knowledge of the complex physical laws that rule our atmosphere to prepare each day’s forecast. Without their technologies and expertise, weather forecasting would be unreliable guesswork. NWS original forecasts are then distributed to the public where commercial apps and self-appointed gatekeepers filter out the substance and relay their versions that will entertain the masses and increase ratings. To bypass this media fluff, you can go directly to the source of the forecast. Just click your region and let the real learning begin: https://www.weather.gov/ Thank you National Weather Service professionals!
The images that follow are presented in chronological order as the season progressed. Various NOAA satellite imagery was used along with weather maps from San Francisco State University to display and explain evolving weather patterns. These 500mb charts are used to show upper level patterns and winds that often dictate weather conditions on the ground.
After a dry October, powerful autumn storms began to form in the north Pacific and aim at the Golden State. Atmospheric rivers seemed to be setting up ahead of these incoming low pressure systems until the lowest sea level pressure ever observed in California was recorded at Crescent City in late November. By December, we seemed well on our way toward what would be another banner water year.
By January, upper level patterns were shifting dramatically toward drought and by February, those ridiculously resilient ridges were locking in place over us, right in the middle of what should have been our wettest months of the year. Huge swaths of California from the coast to the Sierra Nevada received no measurable precipitation in February for the first time since recording began, following an unusually dry January. And for most stations in central and northern California, March was also disappointing. Stations around and beyond the San Francisco Bay Area into the Central Valley and along the central Coast received no precipitation in February. These included San Francisco, Oakland, San Jose, Sacramento, Salinas, Big Sur State Park, and Paso Robles. Southern California stations also recorded well below average precipitation in February (L.A. experienced its 10th driest on record) and most of the state was left at less than 5% of its average for the normally wettest months of January and February combined.
Just when it seemed too late to salvage this rainy season, nature delivered some March and April miracles to southern California that would miss many locations to the north. They arrived as a series of odd upper level lows that became cut off from general circulation patterns. Some of them drifted inland to the north as dry inside sliders and then retrograded southwest back over the ocean to pick up moisture off of southern California. Others spun right down the coast, mostly missing the north and then wandering and wobbling, again, southwest of southern California. As they finally drifted inland from northern Baja or across the southern California bight, these relatively small systems delivered soaking rains throughout southern California and well into the Desert Southwest.
During April, southern California caught up to its average or surpassed the seasonal precipitation totals, while northern California was left stranded in a serious drought year. As an example, Los Angeles accumulated 140% of its average precipitation for November and December, only 8% for January and February, and then 130% for March and April, while central and northern California missed most of those spring downpours. These cutoff lows became much more than the typical weather forecasters’ woes in the spring of 2020.
Though the late rains brought spring wildflower displays to the deserts and tempered what would have been a horrendous early fire season in southern California, they kept northern and central California on the dry side. As if the state had become meteorologically inverted, many southern California coastal stations ended up with twice as much rainfall as San Francisco and other stations around the Bay Area. The state’s northern and central snow packs and runoff into reservoirs (sources for most of California’s water projects) resembled some of the record lows experienced during our recent severe droughts that were finally doused by more recent record wet years.
And so, as this is written in mid July, our spring has turned to summer as a series of high amplitude high pressure ridges and low pressure troughs have been migrating over us, bringing periods of extreme heat, followed by refreshing cool spells, punctuated by high winds . These erratic weather patterns leave us all wondering what is next, knowing that another fire season looms ominous. Will some summer monsoon moisture sneak in from Arizona and Mexico to briefly quench inland southern California and the southern Sierra Nevada? Will Pacific Northwest troughs be strong enough to usher in cool air masses over our state? How long will we have to wait into autumn before the next rainy season returns to snuff out this year’s fire season? If you are reading this several months later, you may already know the answers to these annual scientific guessing games that have become more challenging with our changing climates.
After reviewing this story, you might be interested in comparing this year’s weather events to the average trends during the last century or so. Go to our next story about climate trends in southern California that was inspired by National Weather Service Senior Meteorologist Todd Hall.