Last Sunday's upper level low resulted in a little rain, mostly south of the L.A. basin, but Southern California and much of the West has been dry, dry, dry. How dry? Take a look at this plot of percent of average precipitation for the past 90 days from the Western Regional Climate Center.

Downtown Los Angeles (USC) has not recorded measurable rain for more than a month. The last measurable rain was on December 17 when 0.01 inch recorded. The water year precipitation total for Los Angeles has been stuck on 3.76 inches, which is about 2.5 inches below normal. The Sierra has been especially dry. The Statewide Summary of Snow Water Content for January 18 reported the snowpack at 10% of normal. Remarkably, Mammoth Mountain recorded no natural snow between December 5 and January 19!

The good news is the very stubborn West Coast ridge has finally relented, opening the door to a more zonal flow and a sequence of shortwave troughs. The change in pattern is forecast to produce significant rain and snow over most of the West Coast the next few days. The HPC 5-day Precipitation Forecast indicates up to about 5 inches of precipitation in some areas of the Sierra and North Coast, and over 9 inches in some areas of the Pacific Northwest.

The change in pattern isn't forecast to produce much rain south of Pt. Conception, but at this point just about any amount would be helpful. BUFKIT analysis of WRF Ensemble forecasts for Van Nuys indicate precipitation amounts ranging from about 0.1 inch to 0.5 inch, beginning sometime this evening and ending midday Saturday. The 18z NAM precipitation forecast for Van Nuys projects about 0.25 inch for the storm. Some mountain areas could see somewhat higher precipitation totals, particularly those with a west-facing aspect.

Another shortwave is forecast to move through the area Monday. Model projections differ, but we could get a little rain out of that system as well. We'll see!

Update January 25, 2012 8:00 am PST. Precipitation totals across the area from Monday's system generally ranged from about 0.3 inch to 0.75 inch. Downtown Los Angeles (USC) recorded 0.62 inches for the storm. This combined with the 0.68 inches from Saturday's system boosted the water year total for Los Angles to 5.06 inches, which is about 75% of normal for the date. The medium range models have been all over the place. Yesterday the 12z GFS forecast for Monday morning depicted an upper low and trough on the West Coast, while the ECMWF indicated some ridging. Here's a GFS/ECMWF comparison from San Jose State University Meteorology. Given the recent Sudden Stratospheric Warming (SSW) and rejuvenation of the MJO there's plenty of uncertainty in the medium range. The ECMWF seems to like the idea of a relatively fast-moving trough affecting the West Coast sometime around February 1. We'll see!

Update January 21, 2012 1:30 pm PST. Perhaps because its jet stream dynamics were more favorable than expected, this first system was a little stronger and held together a little better south of Pt. Conception than suggested by the models. Rainfall totals tabulated by the NWS generally ranged from about 0.2 to 0.7 inch in the Los Angeles area, with somewhat higher totals recorded in Ventura County and Santa Barbara County. Model projections have varied on the strength of the system forecast to move through the area on Monday. The 12z NAM projected about 0.4 inch for Van Nuys; the 18z NAM about 0.3 inch, and the 12z GFS about 0.5 inch. The system appears similar to today's, but it looks like the shortwave trough and vortex max may track more directly into Southern California.

More information about Southern California weather and climate can be found using our WEATHER LINKS page.

Year	Nov-Mar AAM	Peak MEI4	Peak MEI Season	Peak ONI	Peak ONI Season	L.A. Rain	GWO Phase Plot
1949-501,2	--	-1.423	APRMAY	-1.7	DJF	9.94	--
1950-511	--	-1.261	NOVDEC	-1.0	NDJ, DJF	8.21	--
1954-551	--	-1.578	MAYJUN (54)	-1.2	ASO	11.94	--
1955-561	--	-2.276	MAYJUN (55)	-2.0	OND	16.00	--
1956-571	--	-1.516	MAYJUN (56)	-0.9	SON, OND	9.54	--
1961-623	-0.513	-1.081	DECJAN	-0.6	ASO, SON	18.79
1962-63	-1.259	-0.849	JANFEB	-0.7	OND, NDJ	8.38
1964-65	-1.145	-1.496	JULAUG	-1.2	SON, OND	13.69
1967-68	-0.770	-1.060	APRMAY	-0.9	JFM	16.58
1970-71	-0.976	-1.898	MARAPR	-1.3	DJF, JFM	12.32
1971-72	-0.173	-1.463	AUGSEP	-1.0	OND	7.17
1973-74	-1.331	-1.937	DECJAN	-2.1	NDJ	14.92
1974-75	-0.842	-1.255	OCTNOV	-0.9	OND	14.35
1975-76	-0.713	-2.000	SEPOCT	-1.7	OND, NDJ	7.22
1984-85	-0.597	-0.743	APRMAY	-1.1	NDJ	12.82
1988-89	-1.139	-1.591	AUGSEP	-1.9	OND, NDJ	8.08
1995-96	-0.227	-0.641	DECJAN	-0.7	OND to JFM	12.46
1998-99	-0.541	-1.219	JANFEB	-1.4	NDJ, DJF	9.09
1999-00	-0.781	-1.228	JANFEB	-1.6	NDJ, DJF	11.57
2000-01	-0.795	-.755	OCTNOV	-0.7	NDJ	17.94
2007-08	-1.010	-1.619	FEBMAR	-1.4	DJF, JFM	13.53
2008-093	-0.596	-.783	SEPOCT	-0.8	DJF	9.08
2010-11	-0.596	-2.037	AUGSEP	-1.4	SON, OND, NDJ	20.20
2011-125	-0.175	-0.980	OCTNOV	-0.7	SON	3.76
1. AAM and AAM tendency anomaly data not available. 2. Based on ONI values beginning with DJF 1949-50. 3. ONI did not meet threshold of 5 consecutive overlapping seasons. 4. MEI values are normalized and may change as new data is added. Specified values were current as of December 31, 2011. 5. Data as of December 31, 2011. ONI may not meet threshold of 5 consecutive overlapping seasons for this episode.

There's been no rainfall recorded at Downtown Los Angeles (USC) since December 17 when 0.01 inch recorded. Los Angeles ended December with 1.01 inch of rain. This is less than half of normal for the month and far less than last December's deluge of 10.23 inches.

Even though December 2011 was somewhat dry, it comes nowhere near setting a record. Since 1877 there have been eight Decembers in which no rain was recorded, and 44 Decembers with 1.01 inches of rain or less.

Downtown begins 2012 with a water year rainfall total of 3.76 inches. Last year we would have said this was near normal, but using the new normals derived from 1981-2010 data the total is 0.56 inch below normal. It has been several years since Downtown Los Angeles (USC) recorded below normal rainfall for the first six months of the water year. The last time was July 1 to December 31, 2007.

In a word the weather for the Rose Parade is expected to be SPECTACULAR. The current NWS point forecast for Pasadena is calling for an overnight low Sunday-Monday of 54 and a high Monday of 83. Click here for the latest NWS forecast for Pasadena.

The MJO has been relatively active this autumn and after going on a two week holiday appeared to be more coherent as it moved into the Western Pacific between Christmas and New Year's. However the NCEP GEFS and several other models forecast the MJO to rapidly diminish in amplitude and eastward propagation.

At the moment the precipitation outlook continues to be on the dry side. We'll see!

The November 30 - December 1, 2011 downslope windstorm felled thousands of trees, produced multi-day power outages and resulted in millions of dollars of damage in valley communities along the San Gabriel Mountains. An initial analysis of the conditions leading up to the event suggest a combination of factors contributed to the strength of the winds. Among them were a highly amplified and energetic north-south upper flow which was evolving into a cutoff upper low over southeastern California; a deepening surface low south of Las Vegas; cold air advection; and a possible inversion near mountain-top level.

More information about Southern California weather and climate can be found using our WEATHER LINKS page.

For the past two years Los Angeles has recorded above normal rainfall over the first six months of the water year (Jul. 1 to Dec. 31). So far this year is following suit.

After a record-setting storm in early October in which Downtown Los Angeles (USC) recorded over an inch or rain, a series of upper level troughs have continued to bump up the rainfall total. The systems have tended to be amplifying upper level troughs that split, typically transforming the southern half of the trough into a difficult-to-forecast cut-off upper level low. The resulting cut-off lows have then tracked over, along, or off the Southern California coast producing varying amounts of rain.

Sunday's system was the fourth to produce measurable rain in Los Angeles this November. A strong cold front produced very heavy rain, resulting in flooded streets and highways and resulting in a host of other weather-related problems. In the middle of it all runners in the PCTR Santa Monica Mountains 9K, 18K, 30K and 50K were running distances up to 31.5 miles on the trails of Pt. Mugu State Park.

Downtown Los Angeles (USC) recorded 0.90 inches for the storm, bringing the water year total to 2.75 inches. This is 1.11 inch above the new 1981-2010 normal for rainfall from July 1 through November 22. Here are some additional (preliminary) precipitation totals from around the area, compiled by the NWS Los Angeles/Oxnard. More than an inch above normal sounds like a lot, but as of today only guarantees Los Angeles precipitation will be above normal through December 12.

Back on July 1 NOAA released the new 1981-2010 climate normals, replacing the 1971-2000 normals that have been used this past decade. Normals serve as a 30 year baseline average of climate variables such as monthly and annual maximum, minimum, and mean temperature; and monthly and annual total precipitation. For example, Downtown Los Angeles' new normal annual precipitation total is now 14.93 inches, down from the 15.14 inches we've been using.

After dropping to -0.503 for July/August, and then to -0.772 for August/September, the September/October value of the Multivariate ENSO Index (MEI) has dropped a bit more to -.968 sigma. This is well within La Nina territory, but almost one sigma less than last year's September/October value. Plots of the Global Wind Oscillation (GWO) for July 1 to November 19, 2011 and the same period last year illustrate the year-to-year difference in the atmosphere's response to La Nina conditions. So far, this year's response is consistent with a more active MJO and a shift toward a more neutral ENSO state.

While there's still a chance of rain in Southern California Thanksgiving Day, the forecast is looking better than it did a few days ago when rain was considered likely. The difficulty in the forecast is yet another upper level trough splitting into a cut-off upper level low. The 12z NAM forecasts the low to remain offshore on Thanksgiving Day, and move into Northern Baja by the late afternoon. The 09z SREF puts the probability of more than 0.01 inch of rain in coastal Southern California for the 12 hours ending 4:00 pm Thursday at 10% - 30% and the chance of more than 0.10 inch of rain at around 10%. A shift in the track of the low toward the coast would significantly increase the chance of rain. We'll see!

More information about Southern California weather and climate can be found using our WEATHER LINKS page.

An unseasonably deep upper level low, unusually strong 170+ kt Pacific jet, and associated cold front combined to produce record-setting rainfall in Southern California Wednesday, October 5. Rainfall totals exceeded 1.0 inch in many areas.

Downtown Los Angeles (USC) recorded 1.15 inches, setting a new record for the date, and kick-starting the area's rainy season to 0.78 inch above normal. Rainfall records for the date were also set for LAX, Long Beach, Camarillo, Santa Barbara and several other locations. It was the first measurable rainfall at Los Angeles since June 17. Here are some preliminary precipitation totals from the NWS Los Angeles/Oxnard,NWS San Joaquin Valley/Hanford and NWS San Diego.

Enhanced convection in the Western Pacific associated with active phase of the MJO, and an extension of the North Pacific Jet caused by a positive East Asian mountain torque event appeared to have contributed to the unseasonable amount of rainfall. As observed by Ed Berry (Atmospheric Insights, Dec. 30, 2007), "...the MJO itself does not generate enough extratropical westerly wind flow to allow the East Asian jet to impact the USA west coast. A strong positive East Asian mountain torque needs to be involved, on average."

The increase in relative AAM shown by the GWO not withstanding, La Nina conditions appear to be consolidating in the equatorial Pacific. This four month sequence of Pacific Ocean Equatorial Temperature anomaly cross sections shows substantial subsurface cooling from July 11 to September 11. The Multivariate ENSO Index (MEI) has dropped from -0.5 for July/August to -0.8 for the August/September season. This drops the MEI from a rank of 16th last month to 13th this month, just above the quintile definition of a moderate La Niña ranking. Last year the MEI for August/September ranked 1st in the record since 1950. This TAO time-longitude plot of SST and SST anomaly shows less cooling than last year on this date.

To get an idea of what the impact of a second year La Nina might be on 2011-12 Winter precipitation in the continental U.S., the ESRL/PSD US Climate Division Dataset Mapping Page was used to construct a map of US composite precipitation anomalies for November to March for year two La Ninas since 1949. The years included were based primarily on MEI rankings, and include 1950-51, 1955-56, 1962-63, 1971-72, 1974-75, 1999-2000 and 2008-09. The base period was 1971-2000.

For this selection of years the coastal Southern California climate division recorded about 5 to 6 inches less precipitation than normal for the period November through March. The percent of normal water year rainfall recorded at Downtown Los Angeles (USC) ranged from a low of 47% (1971, 7.17"), to a high of 106% (1955, 16.00"). The average rainfall at Los Angeles for these years was 70.5% of normal, or 10.7".

More information about Southern California weather and climate can be found using our WEATHER LINKS page.

A dynamic cutoff upper low centered over Southern California produced numerous thunderstorms in Southern California and a broad area of the southwestern U.S. Saturday. The thunderstorms produced thousands of lightning strikes, some heavy downpours, hail and strong winds.

According to an article on Yuba.net over 15,000 lightning strikes were recorded in California over the 24 hour period ending 0600 PDT Sunday. This plot of lightning detections was produced by Tahoe National Forest. (Typically lightning detections include both cloud-cloud and cloud-ground strokes.)

Thunderstorms were widespread in Southern California and several strong thunderstorms were reported by the NWS. This NWS NEXRAD image from about noon on Saturday shows several strong cells including one area flagged as severe. This composite image from WSI/Intellicast.com at 2:45 pm PDT shows estimated cloud tops, cell movement and hail. Half inch hail was reported in several locations by NWS spotters and there was one report of 1.25 inch hail near Lake Los Angeles. A wide swath of enhanced thunderstorm activity developed in the afternoon to the north and northeast of Los Angeles.

Some of the higher rainfall totals reported by the NWS include Lake Palmdale at 0.98 inch; Palmdale 0.84 inch and Lockwood Valley 0.58 inch. Downtown Los Angeles recorded a trace. Here's a NWS Los Angeles/Oxnard tabulation of some rainfall totals from around the area. Here also is a NWS San Joaquin Valley/Hanford tabulation of some rainfall totals in the southern San Joaquin Valley and Sierra.

In a Southern California Weathernotes post in February I commented that the tough question regarding La Niña was whether warming would continue into the NH summer, with neutral ENSO conditions prevailing as we move into autumn; or if the ENSO cycle would swing back toward a La Nina state. It was noted that since 1949, about half of the first year La Nina episodes have continued into a second or third year.

Climate scientist and Multivariate ENSO Index (MEI) codeveloper Klaus Wolter first mentioned the roughly 50/50 chance that La Nina would return following a summer respite in September 2010. A glance at a plot of the extended MEI index, going back to 1871 clearly shows a propensity for a return of La Nina in the year (or years) following stronger La Nina episodes.

In a September 8, 2011 press release NOAA reported that La Nina is back. More precisely, in their September 8 ENSO Diagnostic Discussion CPC states "La Niña conditions have returned and are expected to gradually strengthen and continue into the Northern Hemisphere winter 2011-12." The Multivariate ENSO Index (MEI) has dropped below the weak La Nina threshold, and several oceanic and atmospheric factors are indicative of a reemerging La Nina. There's still a (historically) slight chance of a return to ENSO neutral conditions this fall, but it doesn't appear likely. We'll see!

More information about Southern California weather and climate can be found using our WEATHER LINKS page.

Tuesday a front associated with an unseasonably strong Pacific low pressure system broke rainfall records in much of the northern half of the state. Precipitation records for the date were broken in numerous locations, including Monterey, San Jose, Oakland, San Francisco, Napa, Sacramento, Redding, Eureka and Crescent City. Here are archived copies of record reports from the San Francisco Bay/Monterey NWS Office and the Sacramento NWS Office.

The front and trough produced a few clouds and cooled temperatures in the Los Angeles area, but I didn't see any reports of rain. Downtown Los Angeles (USC) will end the July 1, 2010 to June 30, 2011 water year with 20.20 inches of rain. This is about 133% of the climate normal of 15.14 inches. According to NWS data Camarillo/Oxnard recorded 139% of normal rainfall, Long Beach 145%, Santa Barbara 169% and Palmdale 105%.

Looks like temperatures will be warming up for the July 4th weekend. Temperatures are expected to reach into the 80s at the coast, 90's inland and 100's in the valleys. Desert areas could reach 110 or higher. Models suggest the possibility of some monsoon moisture moving into the area Sunday or Monday, along with a chance of thunderstorms in the mountains and deserts. Check the NWS Los Angeles/Oxnard Office for the latest forecasts and warnings.

More information about Southern California weather and climate can be found using our WEATHER LINKS page.

An unseasonably strong Pacific low pressure system that stalled about 200 NM off the Central Californio coast set new rainfall records from San Francisco to Santa Barbara over the weekend. The N-S oriented front associated with the system was positioned over Santa Barbara and San Luis Obispo counties much of the weekend, resulting in unusually high rainfall totals in some areas. Midday Sunday the upper low began to move east along 35°N, increasing divergence aloft in areas north of Pt. Conception and producing additional precipitation Sunday afternoon and evening.

Saturday a new rainfall record for the date was set in San Francisco; and on Saturday and Sunday new rainfall records were set in Stockton, Modesto, Paso Robles and Santa Maria. Sunday Santa Barbara Airport recorded 1.24 inches of rain, breaking the record for the date, and increasing the station's rainfall total for June to the highest since recordkeeping began in 1941. The dissipating front produced some scattered showers in the Los Angeles area Sunday.

There were some impressive storm totals. Nordhoff Ridge, in Ventura County, recorded 1.07 inches of rain; Refugio Pass, in Santa Barbara County, 2.64 inches; and Rocky Butte, in San Luis Obispo County, 3.94 inches. Downtown Los Angeles (USC) recorded a trace of rain on Sunday, leaving our water year (July 1 to June 30) rainfall total at 20.19 inches. Here is an archived copy of a NWS Los Angeles/Oxnard compilation of some rainfall totals from around the area.

Saturday I did a trail run on the 8000-9000 ft. ridge between Mt. Pinos and Mt. Abel, north of Los Angeles, and was able to observe first-hand the very strong southerly flow associated with this system, and the spectacular wave clouds that resulted.

More information about Southern California weather and climate can be found using our WEATHER LINKS page.

Overall it's been a wet water year in Southern California, but in the fashion of a Mediterranean climate the wet water year has been comprised of a patchwork of wet and dry months.

If it were not for an unusually stormy December in which Downtown Los Angeles recorded 8.32 inches more rain than normal, Los Angeles would be looking at about 76% of normal rainfall this water year instead of 131%. This reduced amount would be more typical of the rainfall recorded in Los Angeles during a La Nina influenced water year.

March was wet, but April and May have been dry. Sunday morning's wet weather added 0.07 inch to May's total for Los Angeles, but the combined April/May rainfall deficit is still about 0.9 inch.

BUFKIT analysis of WRF ensemble data for Van Nuys and LAX suggests tomorrow's storm is likely to produce between 0.1 inch and 0.3 inch of rain in the Los Angeles basin, and perhaps up to 0.4 inch in the San Fernando Valley. SREF Ensemble probabilities and HPC Probabilistic Precipitation Guidance support this estimate.

It won't take a lot of rain to break the record for May 17 at Downtown Los Angeles -- 0.18 inch would do it -- and it would also raise the water year rainfall total for Los Angeles to over 20 inches. The previous precipitation record for May 17 was 0.17", set in 1883. Note: Record for USC Campus (KCQT) is 0.06, set in 1949, but data from Civic Center is used for Downtown Los Angeles records prior to 1921.

There's a chance of more rain Wednesday, and then perhaps again Sunday into Monday. We'll see!

Update Tuesday, May 17, 2011. Rainfall amounts from the storm that affected Los Angeles last night and this morning were generally within the range projected by the WRF ensembles. Downtown Los Angeles (USC) recorded 0.15 inch for the storm, bring the water year total to 19.99 inches. Here's a report compiled by the NWS with some rainfall totals from around the area. Tonight's system is forecast to produce similar rainfall totals. At the moment some drizzle or light rain looks like a possibility in the Los Angeles area Sunday and early Monday.

Update Wednesday, May 18, 2011. Thanks to the system that moved into the area last night, Downtown Los Angeles (USC) recorded additional rainfall Tuesday evening, nudging the rainfall total for May 17 up to 0.18 inch, and breaking the old rainfall record for the date set in 1883. Shower activity appears to be winding down and partly cloudy skies are forecast for Los Angeles this afternoon. Rainfall totals from the second system were generally similar to Tuesday's amounts. Here's a report compiled by the NWS Los Angeles/Oxnard that lists the cumulative rainfall that has resulted from these two storms for a number of stations around the area. The water year total for Downtown Los Angeles (USC) now stands at 20.19 inches.

More information about Southern California weather and climate can be found using our WEATHER LINKS page.

Running in the rain and wind, and splashing through innumerable puddles, Markos Geneti set a new Los Angeles Marathon record in a time of 2:06:35. It was a remarkable performance, in adverse conditions. From 8:00 a.m. to 12:00 p.m. the Mt. Washington RAWS, near the start of the marathon, recorded 0.59 inches of rain; and the Beverly Hills RAWS near mile 17, recorded 1.27 inches. Periods of heavy rain were reported at Santa Monica Airport, near the finish line, through much of the race. According to a report in the Los Angeles Times sports blog, The Fabulous Forum, thousands of runners were evaluated for hypothermia and 25 runners were hospitalized.

Many rainfall records were set around the area Sunday, with some locations recording as much as one-third of a year's normal rainfall in 24 hours! In the early evening rainfall rates of over an inch an hour were recorded in Woodland Hills and Canoga Park. According to a NWS Storm Report, at 6:14 p.m. a flash flood was reported in Woodland Hills with "mud and debris flowing down the street" and "at least four to five vehicles stuck in flowing water."

Downtown Los Angeles (USC) recorded 2.42 inches of rain yesterday, breaking a record set in 1943. Santa Barbara Airport had its wettest day on record, recording 5.23 inches of rain. Here's an archived copy of the NWS Record Report for March 20, listing some of the rainfall records for the day.

Storm totals in excess of 3 inches have been common in Los Angeles, Ventura, Santa Barbara, and San Luis Obispo counties. Higher totals were recorded in many areas. As of 5:00 p.m. the NWS reported that Van Nuys had recorded 6.74 inches of rainfall, Northridge 6.08 inches, Newhall 7.20 inches, Santa Barbara Airport 6.27 inches, San Marcos Pass 10.72 inches, and Gibraltar Dam 11.73 inches. Here's an archived copy of a NWS report with some rainfall and snowfall amounts from around the area.

Downtown Los Angeles made up its rainfall deficit for the month of March and more, increasing its water year rainfall total to 18.55 inches, or about 123% of normal. This makes the 2010-2011 water year the wettest in Los Angeles during a La Nina over the last 60 years, surpassing the totals recorded during the strong La Ninas of 1955-56 (99% of normal) and 1973-74 (106% of normal), and weak La Ninas of 1967-68 (110%) and 2000-01 (118%).

Sunday's heavy rain appears to have had the earmarks of an atmospheric river event. NRL SSM/I IPW imagery (lower right) shows a pre-frontal band of IPW values of 35-40 kg/m2 impinging the coast, NEDIS blended TPW imagery showed a band of ~25 mm TPW extending some 4000 km to the longitude of Hawaii. A BUFKIT cross section based on 12z NAM data for VNY depicted a low level jet (LLJ) structure coinciding with the period of heaviest rainfall. Research by Dr. F. Martin Ralph, et. al., observed that in atmospheric rivers over the eastern Pacific, 75% of the water vapor transport below 500 mb takes place within the lowest 2.25 km and occurs with LLJ wind structure. In addition in cases where a LLJ is present, there was 50% greater precipitation efficiency.

More information about Southern California weather and climate can be found using our WEATHER LINKS page.

Along with January and February, March is one of the big three precipitation months in Southern California in which the average rainfall for Downtown Los Angeles exceeds 3.0 inches. In January we were about 2.5 inches below normal rainfall, and in February about 0.4 inch below normal. So far this March, we're nearly two inches below normal for the month. If it were not for an unusually wet December in which Los Angeles recorded 8.32 inches above normal rainfall, we'd be looking at 50% water year right now instead of over 100%.

If today's 12z NAM and GFS forecasts verify, we could make up that March deficit, and push our water year total up to nearly 120%! According to these numerical forecasts, we could see two to three inches of rain in the Los Angeles area by Monday afternoon, and significantly more in orographically favored foothill and mountain locations. The NAM forecasts moist southerly winds approaching 60 kts at the 5000 ft. level Sunday evening.

BUFKIT analysis of 12z NAM/GFS data generates 2.16/4.11 inches of rain for LAX, 3.56/3.57 inches for Van Nuys, and 4.01/4.20 inches for Santa Barbara. The GFS brings in the second front faster than the NAM, forecasting the onset of heavier rain during the day Sunday, rather than Sunday evening. The 09z SREF puts the probability of more than 1.0 inch of rain in the Los Angeles area for the 24 hour period ending Monday morning at about 90%.

And yes, it does look like there's a chance of rain for the Los Angeles Marathon. Although the heavies rain is forecast to hold off until Sunday afternoon or evening, the 09z SREF pegs the probability of 0.1 inch of rain or more in the Los Angeles area over the 6 hours ending at 11:00 a.m. Sunday at about 70%. BUFKIT analysis of 12z NAM data generates about 0.20 inch at LAX from 8:00 a.m. to noon, with temps in the mid 50's. The GFS says about 0.50 inch over the same period. We'll see!

Be sure to check the NWS Los Angeles/Oxnard web site for the latest forecasts, advisories and warnings. More information about Southern California weather and climate can be found using our WEATHER LINKS page.

The wetter ensemble member forecasts prevailed in last Friday's and Saturday's rain and snow event. Downtown Los Angeles recorded 1.20 inches for the storm. This brought the water year total to 15.78 inches, which is about 104% of normal. Although this might seem unusual in a La Nina influenced rain season, during two of the strongest La Ninas in the past 60 years -- 1955-56 and 1973-74 -- Los Angeles recorded 99% and 106% of normal rainfall. Here's an archived copy of a NWS tabulation of some rainfall totals from around the area from early Friday, February 25, to 10:00 p.m. Saturday, February 26.

The NAM and GFS, as well as the SREF and eWRF ensembles, had a tough time forecasting the rainfall produced by our current scenario -- a relatively shallow, moist westerly flow accompanied by modest jet stream dynamics. As this BUFKIT time-height cross section shows, the wettest eWRF ensemble member depicted a 125 kt jet max overhead, suggesting the models had some difficulty in forecasting the structure and strength of the jet. At best, the models forecast a few hundredths of an inch of rain in the Los Angeles area, but the most recent NWS tabulation of rainfall totals for the event lists many stations with between 0.1 and 0.25 inch. As of 4:00 a.m. this morning, Downtown Los Angeles has recorded 0.16 inches for the storm, bumping the water year total to 105% of normal.

As a result of the westerly flow, snow levels are currently high, but one of the interesting facets of last Friday's storm was the possibility of very low elevation snow. A NWS Winter Weather Advisory issued February 25 for the Santa Monica Mountains Recreation Area forecast the snow level to drop overnight from above 3000' to between 1000' and 1500'. Snow accumulations from 1 to 3 inches were expected. Some low elevation post frontal showers of graupel or snow were reported in the east San Fernando Valley and La Crescenta Saturday afternoon, but based on the conditions on Sandstone Peak (el. 3111'), the snow anticipated in the SMMRA did not occur. It was an especially challenging forecast, pitting pre-frontal warm air advection, against post-frontal cold air advection, falling humidity, and fluctuating regions of snow growth and omega.

Developed in part to help forecasters deal with lake effect snow, BUFKIT includes a number of special features for snow forecasting and visualization. For example, following are two time-height cross sections generated by BUFKIT from NAM data for VNY (Van Nuys) from 4:00 p.m. Friday, February 25. The elevation for the Bourgoiun precipitation type analysis for each cross section has been raised to 2711 feet MSL. The first BUFKIT cross section shows snow growth, omega, temperature, and the projected precipitation amount and type. The second cross section shows the same parameters, but with relative humidity instead of omega. The purple and yellow rectilinear contours are snow growth, and the red and blue contours are omega. The green bars are rain amounts, and the blue bars snow. Some of the things to note in these cross sections are the omega/snow growth "cross hair," freezing level, and rapid decrease in humidity with the frontal passage.

What the discrete NAM forecast can't show is the variability of the forecast situation. In its most recent release BUFKIT added support for SREF and eWRF ensembles. When combined with BUFKIT's precipitation type and other tools, ensemble forecasts can provide much additional information and insight. In this case eWRF ensemble members for VNY exhibited widely varying thermal profiles, regions of snow growth, omega, and humidity. BUFKIT's Bourgoiun precipitation type analysis for the eWRF ensemble members at 8:00 a.m. Saturday morning showed freezing levels as high as 2882' and as low as 1176'. The pattern of post-frontal precipitation was also quite variable.

More information concerning Southern California weather can be found using our WEATHER LINKS page.