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donsutherland1

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  1. Latest EPS and NBE numbers: As the EPS is based on 10:1 ratios, those figures should probably be cut in half given the low ratio snow that is likely due to above freezing temperatures. For example, the high probability of 1" or more snowfall should be read as showing a high probability of measurable snowfall. Wet snow should fall for a time in NYC, but the opportunity for accumulation will likely be limited to periods where it falls moderately. My guess is that a slushy inch remains likely in Central Park.
  2. EPS and NBE information. Note: EPS data is based on 10:1 ratios. Actual ratios will be much lower given the above freezing temperatures during the storm. My guess is that Central Park will likely see a slushy inch of snow while lower Manhattan, Queens, Brooklyn, and Staten Island see a coating. There is still room for minor changes. I remain concerned about the combination of warm soundings and above freezing temperatures.
  3. The period of quiet weather is coming to an end. The region will be impacted by a series of storms over the next seven days. Tomorrow will be increasingly cloudy and cold. Snow and/or mixed precipitation will overspread the region during the afternoon into the evening. Precipitation will quickly become all rain along the coast. Precipitation will end on Sunday possibly as light snow or snow showers. The storm will likely bring a coating to Queens, Brooklyn, and Staten Island, a slushy inch to Central Park, and up to 2" in the Bronx. 3"-6" of snow will fall well north and west of New York City. Following the region's first winter storm, a severe storm could bring a heavy windswept rain to much of the region during the middle of next week. The potential exists for a 1"-3" rainfall with locally higher amounts, damaging winds, and possibly significant coastal flooding. Temperatures could surge toward or into the 50s. Late next week, a genuine Arctic air mass will likely begin pushing into the Pacific Northwest and Northern Plains. Severe cold is likely in the affected region. Afterward, this cold air could try to come eastward. The ENSO Region 1+2 anomaly was +0.8°C and the Region 3.4 anomaly was +2.0°C for the week centered around December 27. For the past six weeks, the ENSO Region 1+2 anomaly has averaged +1.55°C and the ENSO Region 3.4 anomaly has averaged +2.00°C. A basinwide El Niño event is ongoing. The SOI was -6.59 today. The preliminary Arctic Oscillation (AO) was -0.595 today. Strong blocking in the final week of November, as occurred this year, has often been followed by frequent blocking in December and January. On January 3 the MJO was in Phase 2 at an amplitude of 2.301 (RMM). The January 2-adjusted amplitude was 2.276(RMM).
  4. Reminder: Avoid 10:1 Snow Maps. Go to the Soundings. Latest illustration: 12z GFS at 36 hours. The maps show moderate to heavy snow at JFK. The sounding supports rain. The column is above freezing until one reaches 925 mb. The surface temperature is 38°. Based on the soundings, JFK has little or no accumulation of snow rather than the amounts shown on the 10:1 maps. I highlighted the 0°C line for ease of viewing.
  5. Distribution of Daily Snowfall Amounts by Minimum Temperature with Total Precipitation of 0.50" or More and Measurable Snowfall: Distribution of Event Average Snow-to-Liquid Ratios: The mean event average snow-to-liquid ratio was 1.4 (standard deviation: 1.5). The lowest was near 0. The highest was 9.2. This data was taken from the combined climate records for Bridgeport, Islip, New York City, Newark, and Philadelphia. At present, it appears that Central Park's low temperature during the precipitation will likely be 34° or above. NAM and GFS MOS: 34°. NBE: 36° +/- 3°. This historic data also argues for a low ratio and light accumulation of snow for New York City.
  6. National Blend of Models Output (0z and 12z cycles): The 1/5 14z run decreased a little more to 0.5". It shows a minimum temperature of 36° during the precipitation. Any snow that falls in the NYC area will be low- to very low-ratio snow.
  7. Those maps are a huge problem. I've increasingly starting calling out and verifying the extreme maps posted on Twitter. Those posts provide no useful guidance and only serve to undermine professional credibility of meteorologists, many of whom are outstanding, but whose insights and forecasts are drowned out by the noise of the extreme posts, blind rush to be first to make a call, etc. Indeed, a female TV meteorologist from Philadelphia was criticized on social media for not making an early call for snowfall amounts when uncertainty was high. She made a forecast for a coating to an inch in Philadelphia yesterday (her first call). That looks good. Contrast that to the social media maps showing 4"-8" or even 4"-12" in Philadelphia that dated as far back as January 1. Quite bluntly, those who consistently post extreme solutions or earliest calls but wind up wrong over and over again lack skill. They can spin it any way they like, but skill is a function of consistent accuracy. Nothing more. Unfortunately, the public and those who read social media don't realize the absence of skill among those who take sensationalist stands. Thus, the misleading perception that meteorologists 'can't forecast' prevails even as those perceptions are far off the mark.
  8. In terms of the concern about "waffling," there was a lot of good analysis provided by numerous people. Wdrag, Bluewave, Dark Star, among others, provided good insight. Others provided good arguments why the event could be better. It should be noted that people can provide good insight and still be wrong in the end. Forecasting is inherently uncertain and all who engage in it encounter error from time to time. From my vantage point (which has been wrong at times and will again be wrong), there were persistent "red flags" that urged caution from the onset: Overall synoptic pattern, persistent surface temperature projections, emergent soundings data, and risks associated with extreme outlier solutions that lacked strong support. For illustrative purposes to show how these "red flags" came into play, excerpts from some posts follow. One should also read through Bluewave's posts, as he consistently raised issues that are now playing out e.g., the impact of the upstream trough in the Southwest. January 3: Of concern remains surface temperatures that will be above freezing for most or all of the event. Soundings will become increasingly important as the event draws closer, but this still looks to be a wet, low ratio snowfall for NYC and its nearby suburbs. January 3: The importance of recognizing that the upcoming event will be a low- to very low-ratio event in New York City cannot be overstated. Most of the guidance keeps NYC above freezing throughout the storm. While model solutions showing 6"+ snow appear attractive, the early surface temperature forecasts and early soundings suggest that such figures based on a 10:1 ratio will likely be far off the mark. January 4: There was more downside risk than upside risk. Unfortunately, even at this point in time, there still remains somewhat more downside risk than upside risk, namely that the 1" of slushy snow to perhaps 3", if everything went well, could evolve into a coating to an inch-type scenario. The low ratios (high confidence assumption given the consistently forecast temperatures) rendered 10:1 snowfall maps irrelevant. That included individual ensemble maps based on 10:1 ratios. In both cases, the operational and ensemble maps overstated what was likely. For an illustrative example, maps assessing the probability of 4" or more snowfall were actually assessing the probability of 2" or more snow in and around NYC and along the coastal plain, because their 10:1 ratios were not realistic. As a result of the overnight guidance, the probability that New York City's streak without 1" or more daily snowfall, which will reach 690 days today, will continue has increased. January 4: Be wary of snow maps e.g., the 18z NAM's depictions... A significant share of the precipitation is rain or mixed precipitation, not snow. For example, at 75 hours when the NAM is piling on the digital snow, the sounding shows the above freezing layer extending almost to 975 mb with above-freezing surface temperatures. Over New York City's urban heat island, that's not accumulating snow. The precipitation ends as snow, but accumulations will likely be limited. Outlier models for heavy snowfall that lack support should be disregarded given the marginal air mass and historic experience with snowfall at above freezing temperatures in New York City.
  9. I don't know about the timing, as sometimes the guidance rushes things, but I am highly confident that we will get in the teens this winter (probably second half of this month).
  10. Overnight, the NAM finally "woke up" to reality in abandoning its high snowfall amounts that were not supported by its own soundings. The guidance also consolidated toward a minor event in the NYC area and a moderate event well north and west of the City i.e., West Milford, Goshen, Danbury, etc. The coating to 1" scenario for Central Park remains on the table. In fact, the 11z NBE now shows just 0.6" in the Park. The <1" daily snowfall streak will reach 691 days today and could continue through the upcoming storm. Next week's rain and wind storm will be a much higher-impact event for the region.
  11. No. Winter 2001-02 came closest with a minimum temperature of 19.
  12. Latest EPS and NBE information: Be wary of snow maps e.g., the 18z NAM's depictions below: A significant share of the precipitation is rain or mixed precipitation, not snow. For example, at 75 hours when the NAM is piling on the digital snow, the sounding shows the above freezing layer extending almost to 975 mb with above-freezing surface temperatures. Over New York City's urban heat island, that's not accumulating snow. The precipitation ends as snow, but accumulations will likely be limited. Outlier models for heavy snowfall that lack support should be disregarded given the marginal air mass and historic experience with snowfall at above freezing temperatures in New York City.
  13. Generally dry weather will continue through tomorrow. Afterward, a series of storms will impact the region. A storm will bring measurable snowfall to parts of the region Saturday afternoon into Sunday. This appears to be the kind of storm that could bring a general 1" to perhaps 3" of slushy snow to New York City (lowest amounts in Queens, Brooklyn, and Staten Island and highest amounts in the Bronx) with 3"-6" of snow well north and west of New York City. The probability of a significant (6" or greater) snowfall in Boston has increased. There remains a degree of uncertainty in coastal regions, including the New York City area. Following the region's first winter storm, a major storm could bring a heavy windswept rain to much of the region during the middle of next week. The potential exists for a 1"-3" rainfall with locally higher amounts. Temperatures could surge toward or into the 50s. The ENSO Region 1+2 anomaly was +0.8°C and the Region 3.4 anomaly was +2.0°C for the week centered around December 27. For the past six weeks, the ENSO Region 1+2 anomaly has averaged +1.55°C and the ENSO Region 3.4 anomaly has averaged +2.00°C. A basinwide El Niño event is ongoing. The SOI was -5.74 today. The preliminary Arctic Oscillation (AO) was -0.696 today. Strong blocking in the final week of November, as occurred this year, has often been followed by frequent blocking in December and January. On January 2 the MJO was in Phase 2 at an amplitude of 2.276 (RMM). The January 1-adjusted amplitude was 1.959 (RMM).
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