Pub Date : 2018-12-20DOI: 10.15191/NWAJOM.2018.0609
Sean Ernst, Daphne S. LaDue, Alan E. Gerard
For Emergency Managers (EMs), preparations for severe weather have always relied on accurate, well-communicated National Weather Service (NWS) forecasts. As part of their constant work to improve these forecasts, the NWS has recently begun to develop impact-based products that share forecast uncertainty information with EMs, including the Probabilistic Hazard Information (PHI) tool. However, there is a lack of research investigating what forecast uncertainty information EMs understand, and what information needs exist in the current communication paradigm. This study used the Critical Incident Technique to identify themes from incidents involving weather forecast information that went well, or not so well, from the perspective of the EMs responding to them. In total, 11 EMs from a variety of locales east of the Rockies were interviewed—six of whom were county-level, two city, two state, and one from a school district. We found that EMs sought increased forecast detail as a potential event approached in time and built relational trust in the NWS through repeated interactions. EMs had difficulty preparing for events when they did not have details of the expected impacts, or the likelihood of those impacts, for their regions. In summary, EMs are already starting to work in an uncertainty-friendly frame and could be responsive to the impact details and increased forecaster relations proposed with the PHI tool.
{"title":"Understanding emergency manager forecast use in severe weather events.","authors":"Sean Ernst, Daphne S. LaDue, Alan E. Gerard","doi":"10.15191/NWAJOM.2018.0609","DOIUrl":"https://doi.org/10.15191/NWAJOM.2018.0609","url":null,"abstract":"For Emergency Managers (EMs), preparations for severe weather have always relied on accurate, well-communicated National Weather Service (NWS) forecasts. As part of their constant work to improve these forecasts, the NWS has recently begun to develop impact-based products that share forecast uncertainty information with EMs, including the Probabilistic Hazard Information (PHI) tool. However, there is a lack of research investigating what forecast uncertainty information EMs understand, and what information needs exist in the current communication paradigm. This study used the Critical Incident Technique to identify themes from incidents involving weather forecast information that went well, or not so well, from the perspective of the EMs responding to them. In total, 11 EMs from a variety of locales east of the Rockies were interviewed—six of whom were county-level, two city, two state, and one from a school district. We found that EMs sought increased forecast detail as a potential event approached in time and built relational trust in the NWS through repeated interactions. EMs had difficulty preparing for events when they did not have details of the expected impacts, or the likelihood of those impacts, for their regions. In summary, EMs are already starting to work in an uncertainty-friendly frame and could be responsive to the impact details and increased forecaster relations proposed with the PHI tool.","PeriodicalId":44039,"journal":{"name":"Journal of Operational Meteorology","volume":" ","pages":""},"PeriodicalIF":1.1,"publicationDate":"2018-12-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"48742614","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2018-12-14DOI: 10.15191/NWAJOM.2018.0608
J. Cordeira, Molly M. Neureuter, L. Kelleher, Geneva New York William Smith Colleges
Atmospheric rivers (ARs) are a focus of many global hydrometeorological studies and applications. The impacts of ARs along the United States’ West Coast include extreme orographic precipitation that often leads to flooding, flash flooding, debris flows, and other hydrological hazards that necessitate issuance of watches, warnings, and advisories (WWAs) by the National Weather Service (NWS). The objectives of this paper are to quantify and illustrate the relationship between landfalling ARs and high-impact weather events in California by comparing a catalog of landfalling ARs to a 10-year geospatial catalog of WWAs issued by the NWS. NWS WWAs are issued frequently over California in regions of topography (e.g., the northern Sierra Nevada and Transverse Ranges) in association with flooding and winter weather across northern California and flash flooding across southern California. A large majority of cool-season days with WWAs related to flooding (~50– 75%) and winter weather (~60–80%) occur on days with landfalling ARs. Alternatively, landfalling ARs on cool-season days also enhance the likelihood of high-impact weather over different regions of California with greatly increased likelihoods of WWAs relative to climatology as AR intensity increases. ABSTRACT (Manuscript received 26 July 2018; review completed 12 October 2018)
{"title":"Atmospheric Rivers and National Weather Service Watches, Warnings, and Advisories Issued Over California 2007–2016","authors":"J. Cordeira, Molly M. Neureuter, L. Kelleher, Geneva New York William Smith Colleges","doi":"10.15191/NWAJOM.2018.0608","DOIUrl":"https://doi.org/10.15191/NWAJOM.2018.0608","url":null,"abstract":"Atmospheric rivers (ARs) are a focus of many global hydrometeorological studies and applications. The impacts of ARs along the United States’ West Coast include extreme orographic precipitation that often leads to flooding, flash flooding, debris flows, and other hydrological hazards that necessitate issuance of watches, warnings, and advisories (WWAs) by the National Weather Service (NWS). The objectives of this paper are to quantify and illustrate the relationship between landfalling ARs and high-impact weather events in California by comparing a catalog of landfalling ARs to a 10-year geospatial catalog of WWAs issued by the NWS. NWS WWAs are issued frequently over California in regions of topography (e.g., the northern Sierra Nevada and Transverse Ranges) in association with flooding and winter weather across northern California and flash flooding across southern California. A large majority of cool-season days with WWAs related to flooding (~50– 75%) and winter weather (~60–80%) occur on days with landfalling ARs. Alternatively, landfalling ARs on cool-season days also enhance the likelihood of high-impact weather over different regions of California with greatly increased likelihoods of WWAs relative to climatology as AR intensity increases. ABSTRACT (Manuscript received 26 July 2018; review completed 12 October 2018)","PeriodicalId":44039,"journal":{"name":"Journal of Operational Meteorology","volume":"1 1","pages":""},"PeriodicalIF":1.1,"publicationDate":"2018-12-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"42990149","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2018-09-19DOI: 10.15191/NWAJOM.2018.0607
M. Benoit, C. Nowotarski, D. Conlee, L. Wood, League City Texas Nws
This paper describes the forecasting impacts of a partnership between university faculty and students and forecasters in an on-demand supplemental radiosonde observations program in a data-sparse region. Impacts of the supplemental radiosondes and incorporation into forecast practices by forecasters in both severe convective weather and winter precipitation scenarios are described, with considerable influence found in both situations. Results of a data assimilation experiment, wherein the supplemental radiosondes are assimilated into highresolution, convection-allowing regional numerical weather prediction model forecasts are also presented. Although assimilation of the radiosonde has limited results in model forecast skill in convective precipitation events, modest forecast improvements are found in short-range forecasts of low-level temperatures during winter weather events. ABSTRACT (Manuscript received 14 May 2018; review completed 15 August 2018)
{"title":"Impacts of a University-led, On-demand Sounding Program on Human and Numerical Weather Prediction Model Forecasts in an Upper-air Observation Hole","authors":"M. Benoit, C. Nowotarski, D. Conlee, L. Wood, League City Texas Nws","doi":"10.15191/NWAJOM.2018.0607","DOIUrl":"https://doi.org/10.15191/NWAJOM.2018.0607","url":null,"abstract":"This paper describes the forecasting impacts of a partnership between university faculty and students and forecasters in an on-demand supplemental radiosonde observations program in a data-sparse region. Impacts of the supplemental radiosondes and incorporation into forecast practices by forecasters in both severe convective weather and winter precipitation scenarios are described, with considerable influence found in both situations. Results of a data assimilation experiment, wherein the supplemental radiosondes are assimilated into highresolution, convection-allowing regional numerical weather prediction model forecasts are also presented. Although assimilation of the radiosonde has limited results in model forecast skill in convective precipitation events, modest forecast improvements are found in short-range forecasts of low-level temperatures during winter weather events. ABSTRACT (Manuscript received 14 May 2018; review completed 15 August 2018)","PeriodicalId":44039,"journal":{"name":"Journal of Operational Meteorology","volume":" ","pages":""},"PeriodicalIF":1.1,"publicationDate":"2018-09-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"46852577","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2018-06-15DOI: 10.15191/NWAJOM.2018.0606
Christopher M. Gitro, Kansas City Nws, Missouri Pleasant Hill, Michael L. Jurewicz, S. Kusselson, J. Forsythe, S. Kidder, E. Szoke, D. Bikos, Andrew S. Jones, Chad Gravelle, C. Grassotti
The Cooperative Institute for Research in the Atmosphere, via the Joint Polar Satellite System Proving Ground, developed an advectively blended layered precipitable water (ALPW) product that portrays moisture profiles at a common time across the grid. Using water vapor profile retrievals from the National Oceanic and Atmospheric Administration’s Microwave Integrated Retrieval System (MiRS) aboard polar-orbiting spacecraft, the ALPW product is able to depict the moisture distribution for four atmospheric layers. The ALPW layers are advected forward in time every 3-h using Global Forecast System model winds. Advective blending offers a reduction to the visual limitations seen with traditional non-advected layered precpitable water (LPW) imagery, as satellite swath lines and data discontinuities largely are removed. Having the same temporal resolution as LPW imagery, the new ALPW product offers a more continuous and complete picture of the moisture distribution in these four atmospheric layers (surface–850 hPa, 850–700 hPa, 700–500 hPa, and 500–300 hPa). The advected product also is easier for forecasters to interpret as the analysis at a common time and grid makes the ALPW product comparable to operational model guidance. This paper demonstrates the utility of the ALPW product as a situational awareness tool by highlighting the environments associated with three recent high-impact flash flood events. Initial findings indicate that ALPW data have improved the detection capability for tracking deep tropospheric moisture plumes from source regions well-removed from the flash flood locations. ABSTRACT (Manuscript received 18 December 2017; review completed 11 May 2018)
{"title":"Using the Multisensor Advected Layered Precipitable Water Product in the Operational Forecast Environment","authors":"Christopher M. Gitro, Kansas City Nws, Missouri Pleasant Hill, Michael L. Jurewicz, S. Kusselson, J. Forsythe, S. Kidder, E. Szoke, D. Bikos, Andrew S. Jones, Chad Gravelle, C. Grassotti","doi":"10.15191/NWAJOM.2018.0606","DOIUrl":"https://doi.org/10.15191/NWAJOM.2018.0606","url":null,"abstract":"The Cooperative Institute for Research in the Atmosphere, via the Joint Polar Satellite System Proving Ground, developed an advectively blended layered precipitable water (ALPW) product that portrays moisture profiles at a common time across the grid. Using water vapor profile retrievals from the National Oceanic and Atmospheric Administration’s Microwave Integrated Retrieval System (MiRS) aboard polar-orbiting spacecraft, the ALPW product is able to depict the moisture distribution for four atmospheric layers. The ALPW layers are advected forward in time every 3-h using Global Forecast System model winds. Advective blending offers a reduction to the visual limitations seen with traditional non-advected layered precpitable water (LPW) imagery, as satellite swath lines and data discontinuities largely are removed. Having the same temporal resolution as LPW imagery, the new ALPW product offers a more continuous and complete picture of the moisture distribution in these four atmospheric layers (surface–850 hPa, 850–700 hPa, 700–500 hPa, and 500–300 hPa). The advected product also is easier for forecasters to interpret as the analysis at a common time and grid makes the ALPW product comparable to operational model guidance. This paper demonstrates the utility of the ALPW product as a situational awareness tool by highlighting the environments associated with three recent high-impact flash flood events. Initial findings indicate that ALPW data have improved the detection capability for tracking deep tropospheric moisture plumes from source regions well-removed from the flash flood locations. ABSTRACT (Manuscript received 18 December 2017; review completed 11 May 2018)","PeriodicalId":44039,"journal":{"name":"Journal of Operational Meteorology","volume":" ","pages":""},"PeriodicalIF":1.1,"publicationDate":"2018-06-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"47605442","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2018-06-12DOI: 10.15191/NWAJOM.2018.0605
B. Lindner, P. Mohlin, A. Caulder, Aaron Neuhauser
A classification and regression tree analysis for sea fog has been developed using 648 low-visibility (<4.8 km) coastal fog events from 1998–2014 along the South Carolina and Georgia coastline. Correlations between these coastal fog events and relevant oceanic and atmospheric parameters determined the range in these parameters that were most favorable for predicting sea fog formation. Parameters examined during coastal fog events from 1998–2014 included sea surface temperature (SST), air temperature, dewpoint temperature, maximum wind speed, average wind speed, wind direction, inversion strength, and inversion height. The most favorable range in SST for sea fog formation was 10.6–23.9°C. The most favorable gaps between air temperature and SST, dewpoint temperature and SST, and dewpoint temperature and air temperature were found to be –1.7– 2.2°C, 0°C, and 0–2.2°C, respectively. The most favorable range in maximum wind speed was 11.1–20.4 km h-1, and the most favorable wind directions were parallel to the coast or SST isopleths. The most favorable range in inversion height was 70.6–617.2 m, and the most favorable inversion strength was anything >6°C. Utilizing these eight predictors, a forecasting decision tree was created and beta tested during the 2016/2017 sea fog season. The decision tree successfully predicted sea fog on 17 of the 18 dates that it occurred (94%) and successfully predicted a lack of sea fog for 189 of the 194 days where sea fog did not occur (97%). Two of the six incorrect predictions appear to have extenuating circumstances. ABSTRACT (Manuscript received 11 December 2017; review completed 16 April 2018)
{"title":"Development and Testing of a Decision Tree for the Forecasting of Sea Fog Along the Georgia and South Carolina Coast","authors":"B. Lindner, P. Mohlin, A. Caulder, Aaron Neuhauser","doi":"10.15191/NWAJOM.2018.0605","DOIUrl":"https://doi.org/10.15191/NWAJOM.2018.0605","url":null,"abstract":"A classification and regression tree analysis for sea fog has been developed using 648 low-visibility (<4.8 km) coastal fog events from 1998–2014 along the South Carolina and Georgia coastline. Correlations between these coastal fog events and relevant oceanic and atmospheric parameters determined the range in these parameters that were most favorable for predicting sea fog formation. Parameters examined during coastal fog events from 1998–2014 included sea surface temperature (SST), air temperature, dewpoint temperature, maximum wind speed, average wind speed, wind direction, inversion strength, and inversion height. The most favorable range in SST for sea fog formation was 10.6–23.9°C. The most favorable gaps between air temperature and SST, dewpoint temperature and SST, and dewpoint temperature and air temperature were found to be –1.7– 2.2°C, 0°C, and 0–2.2°C, respectively. The most favorable range in maximum wind speed was 11.1–20.4 km h-1, and the most favorable wind directions were parallel to the coast or SST isopleths. The most favorable range in inversion height was 70.6–617.2 m, and the most favorable inversion strength was anything >6°C. Utilizing these eight predictors, a forecasting decision tree was created and beta tested during the 2016/2017 sea fog season. The decision tree successfully predicted sea fog on 17 of the 18 dates that it occurred (94%) and successfully predicted a lack of sea fog for 189 of the 194 days where sea fog did not occur (97%). Two of the six incorrect predictions appear to have extenuating circumstances. ABSTRACT (Manuscript received 11 December 2017; review completed 16 April 2018)","PeriodicalId":44039,"journal":{"name":"Journal of Operational Meteorology","volume":" ","pages":""},"PeriodicalIF":1.1,"publicationDate":"2018-06-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"49185742","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2018-06-08DOI: 10.15191/NWAJOM.2018.0604
T. Schmit, S. Lindstrom, Jordan J. Gerth, M. Gunshor
The Advanced Baseline Imager (ABI) on the Geostationary Operational Environmental Satellite (GOES)-R series has 16 spectral bands. Two bands are in the visible part of the electromagnetic spectrum, four are in the near-infrared, and ten are in the infrared. The ABI is similar to advanced geostationary imagers on other international satellite missions, such as the Advanced Himawari Imager (AHI) on Himawari-8 and -9. Operational meteorologists can investigate imagery from the ABI to better understand the state and evolution of the atmosphere. Various uses of the ABI spectral bands are described. GOES-R was launched on 19 November 2016 and became GOES-16 upon reaching geostationary orbit. GOES-16 is the first in a series of four spacecraft that will host ABI. GOES-16 became operational on 18 December 2017, in the GOES-East location. The ABI improvement is two orders of magnitude more than the legacy GOES imager due to more spectral bands and finer spatial and temporal resolutions. ABSTRACT (Manuscript received 18 October 2017; review completed 5 March 2018)
{"title":"Applications of the 16 spectral bands on the Advanced Baseline Imager (ABI).","authors":"T. Schmit, S. Lindstrom, Jordan J. Gerth, M. Gunshor","doi":"10.15191/NWAJOM.2018.0604","DOIUrl":"https://doi.org/10.15191/NWAJOM.2018.0604","url":null,"abstract":"The Advanced Baseline Imager (ABI) on the Geostationary Operational Environmental Satellite (GOES)-R series has 16 spectral bands. Two bands are in the visible part of the electromagnetic spectrum, four are in the near-infrared, and ten are in the infrared. The ABI is similar to advanced geostationary imagers on other international satellite missions, such as the Advanced Himawari Imager (AHI) on Himawari-8 and -9. Operational meteorologists can investigate imagery from the ABI to better understand the state and evolution of the atmosphere. Various uses of the ABI spectral bands are described. GOES-R was launched on 19 November 2016 and became GOES-16 upon reaching geostationary orbit. GOES-16 is the first in a series of four spacecraft that will host ABI. GOES-16 became operational on 18 December 2017, in the GOES-East location. The ABI improvement is two orders of magnitude more than the legacy GOES imager due to more spectral bands and finer spatial and temporal resolutions. ABSTRACT (Manuscript received 18 October 2017; review completed 5 March 2018)","PeriodicalId":44039,"journal":{"name":"Journal of Operational Meteorology","volume":" ","pages":""},"PeriodicalIF":1.1,"publicationDate":"2018-06-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"46465227","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2016-01-01Epub Date: 2016-06-28DOI: 10.15191/nwajom.2016.0407
Elise V Schultz, Christopher J Schultz, Lawrence D Carey, Daniel J Cecil, Monte Bateman
This study develops a fully automated lightning jump system encompassing objective storm tracking, Geostationary Lightning Mapper proxy data, and the lightning jump algorithm (LJA), which are important elements in the transition of the LJA concept from a research to an operational based algorithm. Storm cluster tracking is based on a product created from the combination of a radar parameter (vertically integrated liquid, VIL), and lightning information (flash rate density). Evaluations showed that the spatial scale of tracked features or storm clusters had a large impact on the lightning jump system performance, where increasing spatial scale size resulted in decreased dynamic range of the system's performance. This framework will also serve as a means to refine the LJA itself to enhance its operational applicability. Parameters within the system are isolated and the system's performance is evaluated with adjustments to parameter sensitivity. The system's performance is evaluated using the probability of detection (POD) and false alarm ratio (FAR) statistics. Of the algorithm parameters tested, sigma-level (metric of lightning jump strength) and flash rate threshold influenced the system's performance the most. Finally, verification methodologies are investigated. It is discovered that minor changes in verification methodology can dramatically impact the evaluation of the lightning jump system.
{"title":"Automated Storm Tracking and the Lightning Jump Algorithm Using GOES-R Geostationary Lightning Mapper (GLM) Proxy Data.","authors":"Elise V Schultz, Christopher J Schultz, Lawrence D Carey, Daniel J Cecil, Monte Bateman","doi":"10.15191/nwajom.2016.0407","DOIUrl":"https://doi.org/10.15191/nwajom.2016.0407","url":null,"abstract":"<p><p>This study develops a fully automated lightning jump system encompassing objective storm tracking, Geostationary Lightning Mapper proxy data, and the lightning jump algorithm (LJA), which are important elements in the transition of the LJA concept from a research to an operational based algorithm. Storm cluster tracking is based on a product created from the combination of a radar parameter (vertically integrated liquid, VIL), and lightning information (flash rate density). Evaluations showed that the spatial scale of tracked features or storm clusters had a large impact on the lightning jump system performance, where increasing spatial scale size resulted in decreased dynamic range of the system's performance. This framework will also serve as a means to refine the LJA itself to enhance its operational applicability. Parameters within the system are isolated and the system's performance is evaluated with adjustments to parameter sensitivity. The system's performance is evaluated using the probability of detection (POD) and false alarm ratio (FAR) statistics. Of the algorithm parameters tested, sigma-level (metric of lightning jump strength) and flash rate threshold influenced the system's performance the most. Finally, verification methodologies are investigated. It is discovered that minor changes in verification methodology can dramatically impact the evaluation of the lightning jump system.</p>","PeriodicalId":44039,"journal":{"name":"Journal of Operational Meteorology","volume":"4 7","pages":"92-107"},"PeriodicalIF":1.1,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5749929/pdf/nihms921286.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"35710808","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}