Sunday evening through Wednesday afternoon, another energetic cutoff upper level low spun showers and thunderstorms into Southern California, increasing water year rainfall totals for many stations to near or above normal. Precipitation amounts varied widely, with some stations recording a few hundredths of an inch or less, and some as much as an inch or more. As was the case with the upper low at the end of September, this system produced a number of strong thunderstorms. A severe thunderstorm warning was issued as a result of a cluster of strong thunderstorms in the Antelope Valley Tuesday evening.

Downtown Los Angeles (USC) was one of those stations that didn't have its rain bucket in the right place. The station recorded only 0.08 inch from Sunday evening to Wednesday afternoon, bringing its water year rainfall total to 0.51 inch, which is about 0.16 below normal. Here is an archived Public Information Statement (PDF) from the NWS with some rainfall totals from around the area.

The Aug/Sep value of the Multivariate ENSO Index (MEI), released October 6, dropped another 0.18 sigma to -1.99. This is the lowest value of the MEI since Jul/Aug of 1955, and ranks the current La Nina as the strongest in the MEI record for the Aug/Sep season. Equatorial SST have continued to cool, and this plot of 5-day TAO/TRITON SST shows anomalies of -2.0°C or greater extending west to nearly the dateline.

Cooling of SSTs in the Central Pacific appears to have been enhanced by strong 850mb easterly winds associated with an MJO which propagated into the Western Pacific over the past 2 weeks and slowly diminished in amplitude. Divergence aloft associated with the MJO appears to have enhanced typhoon and tropical storm development in the Indian Ocean and Western Pacific. CIRA TPW loops show a lot of tropical moisture being injected into an extending Pacific jet. This could amplify rainfall amounts along the west coast of the U.S. the next few days.

There's been some drizzle and light rain in the Los Angeles area this morning. BUFKIT analysis of 12z NAM data for Van Nuys and LAX generates about 0.1 inch of rain late Sunday afternoon and evening. The bulk of the precipitation is forecast to occur in the northern two-thirds of California and into the Pacific Northwest. We'll see!

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

This year it wasn't until July 14th that Downtown Los Angeles topped the 90°F mark, and Woodland Hills the 100°F mark. Through mid August we'd had only one short (four day) heatwave. But it's Southern California, and you knew sooner or later temps would soar.

Since the middle of the month temperatures have been above seasonal norms, and particularly so the last couple of days. Monday and Tuesday, Downtown Los Angeles recorded highs of 98°F and 94°F, and Pierce College in Woodland Hills hit 104°F and then a scorching 111°F. This afternoon temperatures downtown have been a few degrees cooler than yesterday, but at Pierce College temps have been just about as hot as yesterday. The good news is an upper level trough is forecast to move onshore in the western U.S. this weekend. In Southern California this will result in a deeper marine layer, and dramatically cooler temperatures.

Intellicast composite radar shows some strong thunderstorm activity in Southern California this afternoon. In some cases hail is indicated, with tops reaching 50,000 ft.

The rapid cooling of equatorial Pacific SSTs took a bit of a breather at the the beginning of August, with SST departures leveling out in Nino regions 3.4 and 4, and even warming somewhat in Nino regions 1+2 and 3. But subsurface temperatures remained cool, and in the last ten days surface temperatures have once again been on the decrease. Here is a comparison of TAO 5-day SST anomalies for August 14 and August 24. TAO data from August 24 shows SST anomalies of -2°C, or greater, extending from 95°W, nearly to the dateline.

Update 08/27/10. Thursday the high at Downtown Los Angeles (USC) was 87°F. Pierce College in Woodland Hills topped out at 107°F. In the 9:00 hour this morning Pierce College temps are running 11°F to 12°F cooler than yesterday.

Update 08/26/10. Wednesday the high at Downtown Los Angeles (USC) was 90°F. Pierce College in Woodland Hills topped out at 109°F. Today's temps should be a near repeat of yesterday's. Big cool down kicks in on Friday, and continues into Sunday. Looks like inland highs will drop around 10°F (give or take) each day. A warming trend is forecast for next week.

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

Following a 26 day stretch in which the temperature at Downtown Los Angeles was below normal 25 of the days, and several lowest maximum temperature records were set around the area, temperatures have soared, and record high temperatures for the date have been recorded at several locations.

On June 30, Downtown Los Angeles ended the water year about 8% above normal. Some stations in the Los Angeles area recorded more than this and some less. There was a wide range of values. For example, Long Beach Airport was about 20% above normal and Santa Barbara Airport about 23% above; but Camarillo Airport reported 31% below normal rainfall. Here's an AHPS graphic showing the percent of normal precipitation in California and the Southwest for the year ending July 1 at 12z.

Equatorial Pacific SSTs have generally continued to cool. According to the CPC's Weekly ENSO Update, issued July 12, the latest weekly SST departures were -1.3°C (Niño1+2), -1.0°C (Niño 3), -0.8°C (Niño 3.4), and -0.4°C (Niño 4). According to the CPC, La Niña conditions occur "when the monthly Niño3.4 OISST departures meet or exceed -0.5°C along with consistent atmospheric features. These anomalies must also be forecasted to persist for 3 consecutive months."

Reflecting the transition from El Nino to La Nina conditions, the Multivariate ENSO Index (MEI) for May-June experienced an unprecedented drop for the time of year, decreasing nearly 1 standard deviation to a value of -0.41. In addition, the Global Wind Oscillation (GWO) has orbited about -2 SD down on the La Nina side of the phase space plot, and with the atmosphere in a generally low momentum state, may be in that neighborhood for a while.

The most recent IRI ENSO Update, released July 15, projects "an approximately 80% probability for continuing La Niña conditions, and a 20% probability for returning neutral ENSO conditions. "

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

Equatorial Pacific SSTs have continued to cool and TAO/TRITON data shows -1.0°C or greater anomalies extending from 95°W to beyond 150°W. According to the CPC's Weekly ENSO Update, issued June 21, the latest weekly SST departures were -0.7°C (Niño1+2), -0.6°C (Niño 3), -0.5°C (Niño 3.4), and 0.0°C (Niño 4). An anomaly of -0.5°C in the Niño 3.4 region is the threshold for La Nina conditions.

The Global Wind Oscillation (GWO) has spiraled well into La Niña territory. The global relative atmospheric angular momentum anomaly is at its lowest value since March 2008, during the La Niña of 2007-2008.

Based on equatorial Pacific SSTs, section plots, tradewinds and cloudiness; and the GWO and AAM; a transition to La Nina conditions appears to be underway.

It looks like Downtown Los Angeles (USC) will likely end the July 1 - June 30 water year having recorded 16.36 inches of rain. This is more than an inch above the 1971-2000 annual climate norm of 15.14 inches.

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

Woodland Hills (Pierce College) topped the 90° mark for the first time this year Memorial Day weekend, and after cooling a few degrees during the week, temperatures are back into the 90's this afternoon. A quick look at temps around the area shows temps near 70 on the coast; 80's to 90's in the valleys, and triple digits in the deserts.

Reflecting the transition to ENSO neutral conditions, the Multivariate ENSO Index (MEI) for April-May declined to 0.54. According to the CPC's Weekly ENSO Update, issued June 1, the latest weekly SST departures are -0.6°C (Niño1+2), -0.4°C (Niño 3), -0.2°C (Niño 3.4), and 0.4°C (Niño 4).

In his May 2010 MEI discussion Klaus Wolter projected the probability of a La Nina event emerging by the end of 2010 at roughly 50%. In it's May 2010 ENSO Quick Look, the International Research Institute for Climate and Society (IRI) put the probability of La Nina conditions from the August-October season through the remainder of 2010 at 42%. We'll see!

Downtown Los Angeles (USC) has recorded 16.36 inches of rain since the water year began July 1. This is more than an inch above the 1971-2000 annual climate norm of 15.14 inches. The water year ends June 30. Climatology and current forecasts suggest it is unlikely that this total will change by more than a hundredth or two before the end of the month.

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

During the last month the 2009-10 El Niño has essentially transitioned to ENSO neutral conditions. Over the course of the event, the Multivariate ENSO Index (MEI) peaked in JAN/FEB at 1.5, and the Oceanic Nino Index (ONI) peaked in NDJ at 1.8. The mean 5-day averaged November 1 to March 31 relative AAM anomaly was 0.304. The strongest El Niño forcing appeared to have occurred in late January after the active phase of the Madden-Julian Oscillation (MJO) enhanced El Nino convection in the equatorial Pacific. Here's a chart comparing the 2009-10 El Niño to 17 other warm ENSO episodes that have occurred since 1950.

Dynamical and statistical ENSO model forecasts suggest the possibility that equatorial Pacific SSTs will continue to decline, leading to weak to moderate La Niña conditions by late Summer or Fall. A return to El Niño conditions does not appear likely, but cannot be ruled out. In his May MEI discussion, Klaus Wolter points out that the 1957-1958 El Nino, an analog to the 2009-2010 El Niño, rebounded after dropping into neutral territory.

Downtown Los Angeles (USC) has recorded 16.31 inches of rain since the water year began July 1. This is more than an inch above the 1971-2000 annual climate norm of 15.14 inches. Recent runs of the GFS and ECMWF show a negatively tilted trough deepening and moving onshore early next week. At this point it looks like there's a pretty good chance of showers north of Pt. Conception, but only a slight chance down here. We'll see!

Update 05/18/10. Stations in the Los Angeles area generally recorded under a tenth of an inch from this system. Some isolated totals of about 0.25 inch were recorded in Ventura and Santa Barbara county, and Rocky Butte in San Luis Obispo recorded 0.48 inch. Here is an archived copy of a NWS Public Information Statement with some rainfall totals from around the area.

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

Following several weeks of dry weather, a shift to a wetter pattern brought much needed rain and snow to California this past week. The pattern change was apparently induced by MJO enhancement of El Niño convection in the equatorial Pacific.

Downtown Los Angeles recorded 1.78 inches of rain from Thursday to Sunday, bringing the water year total to 4.81 inches. This is about 2.20 inches above normal for the date. Rainfall totals generally ranged from 2 to 4 inches in the basin and valleys, and 2 to 6 inches in the mountains. Here's an archived copy of a NWS Public Information Statement with rainfall totals from around the area.

Will the current El Niño produce the expected seasonal impacts in Southern California? A new tool that can help gain some insight into the linkage of climate and weather is the Global Wind Oscillation (GWO) phase space plot. Ed Berry repeatedly demonstrated the usefulness of this tool in his blog Atmospheric Insights. Although the blog has been discontinued, its content remains a valuable resource.

The GWO is a recurring subseasonal phenomenon that involves the transport and interchange of momentum in the earth-atmosphere system. It encompasses the MJO and occurs on a similar timescale. Analogous to the MJO phase space plot, but based on a framework of atmospheric angular momentum (AAM), the GWO phase space plot is a measure global relative atmospheric angular momentum and it's tendency. For details, see Weickmann & Berry, 2008.

Relative AAM is generally positive during an El Niño and negative during a La Nina. Relative AAM is correlated with rain season precipitation in Southern California*, and can be helpful in assessing potential El Niño impacts. The following November to March GWO phase plots show the distinctly different behavior of the GWO during the strong El Niño of 1997-98, and the strong La Nina of 1973-74:

GWO El Niño 1997-1998	GWO La Niña 1973-1974
Click for larger image	Click for larger image

In a decade characterized by quirky El Niños, the El Niño of 2009-10 has been acting like another odd one. From a Southern California perspective, the concern has been that it might be like the El Niño of 2006-07 when Downtown Los Angeles recorded only 3.21" of rain over the water year. In the early stages of the El Niño of 2006 strong convection developed in the Indian Ocean during November, but an MJO did not develop until a second round of Indian Ocean convection occurred in mid December. Relative AAM remained negative, and in terms of the atmosphere, the 2006 El Niño didn't make it to 2007.

This year, Indian Ocean convection did spawn an MJO which eventually enhanced El Niño convection near the dateline. Significant momentum was added to the mid-latitudes of the Northern Hemisphere, energizing the westerlies and contributing to the pattern change that resulted in our recent wet weather. However, the increase in mid-latitude AAM has been mostly offset by negative anomalies at higher latitudes. Following are the GWO phase space plots for the current rain season to date, and the quirky El Niño of 2006-07.

GWO El Niño 2009-2010	GWO El Niño 2006-2007
Click for larger image	Click for larger image

So where do we go from here?. For at least a few days the storm track has shifted north. It appears the GWO might be starting an orbit that will take it farther into the El Niño side of the phase space. Several MJO forecasts show the next MJO cycle shortcutting it's orbit back into the Western Pacific. In the 6-10 day period, the GEFS ensemble MJO forecast indicates enhancement of equatorial convection around 90E, and suppression (by the MJO contribution) of El Niño convection near the dateline. This could modify any short term response of the El Niño signal and the GWO, once again reducing AAM.

Below are the GWO phase plots for two El Niños with ONI and MEI values comparable to the current El Niño. In the 1986-87 El Niño, November to March AAM averaged 0.02, and it wasn't until February that the GWO climbed out of the AAM doldrums. That water year Los Angeles recorded 7.66 inches of rain. On the other hand, in the 1994-95 El Niño, November to March AAM averaged 0.76. In mid December the GWO began to reflect an ocean-atmosphere coupled El Niño response, and Los Angeles went on to record 24.35 inches of rain for the water year. At the moment it looks like Southern California might not be as dry as 1986-87, but probably not as wet as 1994-95. We'll see!

GWO El Niño 1986-1987	GWO El Niño 1994-1995
Click for larger image	Click for larger image

*1958-2008 Precipitation/AAM correlation plot generated using US Climate Division Dataset Seasonal Correlation Page.

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

Compared to last week, GFS and ECMWF runs this week have been much drier in Southern California, with most of the activity focused on the Pacific Northwest. No significant rain is forecast here next week, and both the 6-10 and 8-14 day forecasts project below average precipitation for Southern California.

Recent runs of the GFS show the East Asian jet pumping up a huge, high amplitude ridge in the central Pacific around the dateline, but the resulting downstream trough, jet energy and storm track are forecast to remain above about 40°N.

Model performance has not been the best in recent weeks, and generally suffers during seasonal transitions. However, if the 12z GFS forecast is on the mark, March rainfall for Downtown Los Angeles (USC) would fall well below the 3.14 inch norm. Since normal April rainfall is 0.83 inches, and May only 0.31 inches, beyond March it becomes increasingly unlikely that a big rain event will significantly boost our rainfall total.

Since November 1, Downtown Los Angeles has recorded 8.80 inches of precipitation. This is consistent with the mean November-March precipitation for coastal Southern California during 9 La Niña events from 1948 to the present. (See the composite precipitation map in Weathernotes for October 31, 2008.) The water year total for Los Angeles is now 3.32 inches below normal.

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

Downtown Los Angeles (USC) happened to be under the right cloud yesterday, and recorded 0.02 inch of rain. There's a continuing chance of showers in Southern California through the weekend. The area could use some rain. The last storm to produce more than a couple tenths of inch of rain at Downtown Los Angeles was back on February 24, 2008 -- more than eight months ago.

Last year, California's rain season might have been scripted by Dr. Jekyll and Mr. Hyde. Lowland rain totals and the Sierra snowpack were well above normal through the end of February, and then the spigot was turned off. The storm track shifted north, and California had its driest March to May on record. (The March 29, 2008 post in Ed Berry's Atmospheric Insights blog describes the events that may have led to and maintained this shift.)

Which rain season personality will emerge this Winter? Earlier this year the equatorial Pacific tried to transition to El Nino, but the atmosphere didn't cooperate. As measured by the Multivariate ENSO Index (MEI), the ENSO state has returned to the weak La Nina threshold. And as measured by the Global Wind Oscillation (GWO), an uncooperative atmosphere has continued to cycle through a La Nina base state.

This suggests a winter precipitation outlook with a La Nina flavor -- similar to last year. This precipitation map, generated by the ESRL-PSD Composite ENSO plots page, shows the mean November-March precipitation for the U.S. during 9 La Niña events from 1948 to the present. The average La Niña rainfall indicated for coastal Southern California is in the 7.0-10.5 inch range. Last season's November-March rainfall in Downtown Los Angeles was about 12 inches.

Here's the current Nov-Dec-Jan precipitation outlook issued October 16 by the Climate Prediction Center. The "EC" means an equal chance of below normal, near normal, or above normal precipitation. The IRI Multi Model Seasonal Forecast for Nov-Dec-Jan is similar. We'll see!

Update 11/4/08. Here are the NWS Public Information Statements with preliminary rainfall totals for the period from Friday evening to Sunday morning, and from overnight last night to 10:00 a.m. this morning. The current Climate Prediction Center 6-10 day and 8-14 Precipitation Outlooks project below normal rainfall for Southern California. In Atmospheric Insights, Ed Berry paints a scenario with an extended North Pacific Jet collapsing into a strong western U.S. trough in the week 2-3 timeframe. We'll see!

Update 11/1/08. Did a trail run this morning in the Pt. Mugu State Park Area. Over the course of 3+ hours watched 2-3 waves of convection march northeast from the Santa Barbara Channel across the Oxnard Plain. We were showered on a few times, but were very happy to be east of these training T-storms and heavy rain. Here is a NWS Public Information Statement with some rainfall totals as of 11:00 a.m.

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