Pub Date : 2024-04-22DOI: 10.1175/bams-d-23-0123.1
Malcolm Maas, Timothy Supinie, Andrew Berrington, Samuel Emmerson, Ava Aidala, Michael Gavan
Abstract Given inconsistencies in reporting methods and general lack of documentation, the creation of a unified tornado database across the world has been an elusive target for severe weather climatology purposes and historical interest. Previous online tornado documentation has also often been inconsistent or is now defunct. Many individual countries or continents maintain tornado information through either government-sponsored or independent organizations. The Tornado Archive was developed to create a first-of-its-kind digitized synthesis of worldwide tornado documentation, using the most complete sources of information available for regions known to be tornadically active. Spatial and temporal trends in tornado occurrence and reporting can be visualized through an interactive user interface with a variety of filtering methods and environmental reanalysis datasets, such as ERA5. The additional data introduced using Thomas Grazulis’ Significant Tornadoes may be beneficial for tornado climatology studies over the United States. The Tornado Archive is also intended to be a collaborative exercise, with clear data attribution and open avenues for augmentation, and the creation of a common data model to store the tornado information will assist in maintaining and updating the database. In this work, we document the methods necessary for creating the Tornado Archive database, provide broader climatological analysis of spatiotemporal patterns in tornado occurrence, and outline potential use cases for the data. We also highlight its key limitations, and emphasize the need for further international standardization of tornado documentation.
摘要 由于报告方法的不一致和文献资料的普遍缺乏,建立一个全球统一的龙卷风数据库一直是一个难以实现的目标,既不利于恶劣天气气候学的研究,也不利于历史研究。以前的在线龙卷风文献也经常不一致或现已失效。许多国家或大陆通过政府赞助或独立组织来维护龙卷风信息。龙卷风档案的开发旨在利用已知龙卷风活跃地区最完整的信息来源,创建一个同类首创的全球龙卷风文献数字化综合资料库。龙卷风发生和报告的空间和时间趋势可通过交互式用户界面进行可视化,该界面采用了多种过滤方法和环境再分析数据集(如ERA5)。使用 Thomas Grazulis 的 "重要龙卷风 "引入的额外数据可能对美国龙卷风气候学研究有益。龙卷风档案 "也是一项合作性工作,数据归属清晰,扩充途径开放,创建一个通用数据模型来存储龙卷风信息将有助于数据库的维护和更新。在这项工作中,我们记录了创建龙卷风档案数据库的必要方法,对龙卷风发生的时空模式进行了更广泛的气候学分析,并概述了数据的潜在用例。我们还强调了其主要局限性,并强调了进一步实现龙卷风文献国际标准化的必要性。
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Pub Date : 2024-04-22DOI: 10.1175/bams-d-23-0163.1
Mitchell Bushuk, Sahara Ali, David A. Bailey, Qing Bao, Lauriane Batté, Uma S. Bhatt, Edward Blanchard-Wrigglesworth, Ed Blockley, Gavin Cawley, Junhwa Chi, François Counillon, Philippe Goulet Coulombe, Richard I. Cullather, Francis X. Diebold, Arlan Dirkson, Eleftheria Exarchou, Maximilian Göbel, William Gregory, Virginie Guemas, Lawrence Hamilton, Bian He, Sean Horvath, Monica Ionita, Jennifer E. Kay, Eliot Kim, Noriaki Kimura, Dmitri Kondrashov, Zachary M. Labe, WooSung Lee, Younjoo J. Lee, Cuihua Li, Xuewei Li, Yongcheng Lin, Yanyun Liu, Wieslaw Maslowski, François Massonnet, Walter N. Meier, William J. Merryfield, Hannah Myint, Juan C. Acosta Navarro, Alek Petty, Fangli Qiao, David Schröder, Axel Schweiger, Qi Shu, Michael Sigmond, Michael Steele, Julienne Stroeve, Nico Sun, Steffen Tietsche, Michel Tsamados, Keguang Wang, Jianwu Wang, Wanqiu Wang, Yiguo Wang, Yun Wang, James Williams, Qinghua Yang, Xiaojun Yuan, Jinlun Zhang, Yongfei Zhang
Abstract This study quantifies the state-of-the-art in the rapidly growing field of seasonal Arctic sea ice prediction. A novel multi-model dataset of retrospective seasonal predictions of September Arctic sea ice is created and analyzed, consisting of community contributions from 17 statistical models and 17 dynamical models. Prediction skill is compared over the period 2001–2020 for predictions of Pan-Arctic sea ice extent (SIE), regional SIE, and local sea ice concentration (SIC) initialized on June 1, July 1, August 1, and September 1. This diverse set of statistical and dynamical models can individually predict linearly detrended Pan-Arctic SIE anomalies with skill, and a multi-model median prediction has correlation coefficients of 0.79, 0.86, 0.92, and 0.99 at these respective initialization times. Regional SIE predictions have similar skill to Pan-Arctic predictions in the Alaskan and Siberian regions, whereas regional skill is lower in the Canadian, Atlantic, and Central Arctic sectors. The skill of dynamical and statistical models is generally comparable for Pan-Arctic SIE, whereas dynamical models outperform their statistical counterparts for regional and local predictions. The prediction systems are found to provide the most value added relative to basic reference forecasts in the extreme SIE years of 1996, 2007, and 2012. SIE prediction errors do not show clear trends over time, suggesting that there has been minimal change in inherent sea ice predictability over the satellite era. Overall, this study demonstrates that there are bright prospects for skillful operational predictions of September sea ice at least three months in advance.
摘要 本研究对迅速发展的北极海冰季节性预测领域的最新技术进行了量化。建立并分析了一个新颖的多模式数据集,该数据集由 17 个统计模式和 17 个动力学模式的群体贡献组成,对北极 9 月海冰的季节性预测进行了回顾性分析。比较了 2001-2020 年期间对 6 月 1 日、7 月 1 日、8 月 1 日和 9 月 1 日初始化的泛北极海冰范围(SIE)、区域 SIE 和当地海冰浓度(SIC)的预测能力。这套不同的统计和动力学模式可以单独预测线性去趋势的泛北极海冰面积异常,多模式中值预测在这些初始化时间的相关系数分别为 0.79、0.86、0.92 和 0.99。在阿拉斯加和西伯利亚地区,区域 SIE 预测与泛北极预测的技能相似,而在加拿大、大西洋和北极中部地区,区域技能较低。在泛北 SIE 的预测中,动力学模式和统计模式的技能基本相当,而在区域和局地预测中,动力学模式优于统计模式。在 1996 年、2007 年和 2012 年的极端 SIE 年,相对于基本参考预报,预测系统提供了最大的附加值。SIE预测误差没有显示出明显的时间趋势,表明卫星时代海冰固有的可预测性变化极小。总之,这项研究表明,至少提前三个月对九月海冰进行熟练的业务预测前景广阔。
{"title":"Predicting September Arctic Sea Ice: A Multi-Model Seasonal Skill Comparison","authors":"Mitchell Bushuk, Sahara Ali, David A. Bailey, Qing Bao, Lauriane Batté, Uma S. Bhatt, Edward Blanchard-Wrigglesworth, Ed Blockley, Gavin Cawley, Junhwa Chi, François Counillon, Philippe Goulet Coulombe, Richard I. Cullather, Francis X. Diebold, Arlan Dirkson, Eleftheria Exarchou, Maximilian Göbel, William Gregory, Virginie Guemas, Lawrence Hamilton, Bian He, Sean Horvath, Monica Ionita, Jennifer E. Kay, Eliot Kim, Noriaki Kimura, Dmitri Kondrashov, Zachary M. Labe, WooSung Lee, Younjoo J. Lee, Cuihua Li, Xuewei Li, Yongcheng Lin, Yanyun Liu, Wieslaw Maslowski, François Massonnet, Walter N. Meier, William J. Merryfield, Hannah Myint, Juan C. Acosta Navarro, Alek Petty, Fangli Qiao, David Schröder, Axel Schweiger, Qi Shu, Michael Sigmond, Michael Steele, Julienne Stroeve, Nico Sun, Steffen Tietsche, Michel Tsamados, Keguang Wang, Jianwu Wang, Wanqiu Wang, Yiguo Wang, Yun Wang, James Williams, Qinghua Yang, Xiaojun Yuan, Jinlun Zhang, Yongfei Zhang","doi":"10.1175/bams-d-23-0163.1","DOIUrl":"https://doi.org/10.1175/bams-d-23-0163.1","url":null,"abstract":"Abstract This study quantifies the state-of-the-art in the rapidly growing field of seasonal Arctic sea ice prediction. A novel multi-model dataset of retrospective seasonal predictions of September Arctic sea ice is created and analyzed, consisting of community contributions from 17 statistical models and 17 dynamical models. Prediction skill is compared over the period 2001–2020 for predictions of Pan-Arctic sea ice extent (SIE), regional SIE, and local sea ice concentration (SIC) initialized on June 1, July 1, August 1, and September 1. This diverse set of statistical and dynamical models can individually predict linearly detrended Pan-Arctic SIE anomalies with skill, and a multi-model median prediction has correlation coefficients of 0.79, 0.86, 0.92, and 0.99 at these respective initialization times. Regional SIE predictions have similar skill to Pan-Arctic predictions in the Alaskan and Siberian regions, whereas regional skill is lower in the Canadian, Atlantic, and Central Arctic sectors. The skill of dynamical and statistical models is generally comparable for Pan-Arctic SIE, whereas dynamical models outperform their statistical counterparts for regional and local predictions. The prediction systems are found to provide the most value added relative to basic reference forecasts in the extreme SIE years of 1996, 2007, and 2012. SIE prediction errors do not show clear trends over time, suggesting that there has been minimal change in inherent sea ice predictability over the satellite era. Overall, this study demonstrates that there are bright prospects for skillful operational predictions of September sea ice at least three months in advance.","PeriodicalId":9464,"journal":{"name":"Bulletin of the American Meteorological Society","volume":"2 1","pages":""},"PeriodicalIF":8.0,"publicationDate":"2024-04-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140636671","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2024-04-22DOI: 10.1175/bams-d-24-0095.1
Matthew C. Wheeler, Hanh Nguyen, Chris Lucas, Zhi-Weng Chua, Simon Grainger, David A. Jones, Michelle L. L'Heureux, Ben Noll, Tristan Meyers, Nicolas C. Fauchereau, Alexandre Peltier, Thea Turkington, Hyung-Jin Kim, Takafumi Umeda
"Making Progress on the Operational Alerting of El Niño and La Niña in a Warming World" published on 22 Apr 2024 by American Meteorological Society.
{"title":"Making Progress on the Operational Alerting of El Niño and La Niña in a Warming World","authors":"Matthew C. Wheeler, Hanh Nguyen, Chris Lucas, Zhi-Weng Chua, Simon Grainger, David A. Jones, Michelle L. L'Heureux, Ben Noll, Tristan Meyers, Nicolas C. Fauchereau, Alexandre Peltier, Thea Turkington, Hyung-Jin Kim, Takafumi Umeda","doi":"10.1175/bams-d-24-0095.1","DOIUrl":"https://doi.org/10.1175/bams-d-24-0095.1","url":null,"abstract":"\"Making Progress on the Operational Alerting of El Niño and La Niña in a Warming World\" published on 22 Apr 2024 by American Meteorological Society.","PeriodicalId":9464,"journal":{"name":"Bulletin of the American Meteorological Society","volume":"96 1","pages":""},"PeriodicalIF":8.0,"publicationDate":"2024-04-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140636933","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2024-04-18DOI: 10.1175/bams-d-23-0085.1
Hui Yu, Guomin Chen, Wai-Kin Wong, Jonathan L. Vigh, Chi-kin Pan, Xiaoqin Lu, Jun A. Zhang, Jie Tang, Kun Zhao, Peiyan Chen, Zifeng Yu, Mengqi Yang, Jason Dunion, Zheqing Fang, Xiaotu Lei, Ajit Tyagi, Lianshou Chen
Abstract The Typhoon Landfall Forecast Demonstration Project (TLFDP) (2010–2022) was an international cooperative scientific project conducted under the framework of the WMO. The primary objectives of the TLFDP were to enhance the capability of tropical cyclone (TC) forecasters, and support related decision-makers in effective utilization of the most advanced forecasting techniques for the ultimate purpose of reducing and preventing disasters associated with TC landfall. Forty agencies/organizations/projects globally participated in the activities of the TLFDP following its inception in 2010, although the primary focus was on landfalling TCs in the western North Pacific. The TLFDP facilitated collaborations and workshops that realized notable achievements in four key areas: 1) the collection, production, and sharing of TC data; 2) the development and application of TC forecast verification metrics; 3) research on TC forecast skill; and 4) development of new techniques for TC forecasting. An obvious outcome was the shift from prediction of TC features, including track and intensity, toward prediction of TC impacts with more probabilistic conception. The final years of the project also promoted increasing application of artificial intelligence and machine learning techniques in various techniques for analysis and forecasting of TCs. Although the TLFDP ended in 2022, its core activities have continued to be extended through new WMO projects and regional cooperative initiatives.
{"title":"WMO Typhoon Landfall Forecast Demonstration Project (2010–2022): A Decade of Transition from Track Forecasts to Impact Forecasts","authors":"Hui Yu, Guomin Chen, Wai-Kin Wong, Jonathan L. Vigh, Chi-kin Pan, Xiaoqin Lu, Jun A. Zhang, Jie Tang, Kun Zhao, Peiyan Chen, Zifeng Yu, Mengqi Yang, Jason Dunion, Zheqing Fang, Xiaotu Lei, Ajit Tyagi, Lianshou Chen","doi":"10.1175/bams-d-23-0085.1","DOIUrl":"https://doi.org/10.1175/bams-d-23-0085.1","url":null,"abstract":"Abstract The Typhoon Landfall Forecast Demonstration Project (TLFDP) (2010–2022) was an international cooperative scientific project conducted under the framework of the WMO. The primary objectives of the TLFDP were to enhance the capability of tropical cyclone (TC) forecasters, and support related decision-makers in effective utilization of the most advanced forecasting techniques for the ultimate purpose of reducing and preventing disasters associated with TC landfall. Forty agencies/organizations/projects globally participated in the activities of the TLFDP following its inception in 2010, although the primary focus was on landfalling TCs in the western North Pacific. The TLFDP facilitated collaborations and workshops that realized notable achievements in four key areas: 1) the collection, production, and sharing of TC data; 2) the development and application of TC forecast verification metrics; 3) research on TC forecast skill; and 4) development of new techniques for TC forecasting. An obvious outcome was the shift from prediction of TC features, including track and intensity, toward prediction of TC impacts with more probabilistic conception. The final years of the project also promoted increasing application of artificial intelligence and machine learning techniques in various techniques for analysis and forecasting of TCs. Although the TLFDP ended in 2022, its core activities have continued to be extended through new WMO projects and regional cooperative initiatives.","PeriodicalId":9464,"journal":{"name":"Bulletin of the American Meteorological Society","volume":"59 1","pages":""},"PeriodicalIF":8.0,"publicationDate":"2024-04-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140629490","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2024-04-18DOI: 10.1175/bams-d-23-0031.1
Jannick Fischer, Johannes M. L. Dahl, Brice E. Coffer, Jana Lesak Houser, Paul M. Markowski, Matthew D. Parker, Christopher C. Weiss, Alex Schueth
Abstract Over the last decade, supercell simulations and observations with ever increasing resolution have provided new insights into the vortex-scale processes of tornado formation. This article incorporates these and other recent findings into the existing three-step model by adding an additional fourth stage. The goal is to provide an updated and clear picture of the physical processes occurring during tornadogenesis. Specifically, we emphasize the importance of the low-level wind shear and mesocyclone for tornado potential, the organization and interaction of relatively small-scale pre-tornadic vertical vorticity maxima, and the transition to a tornado-characteristic flow. Based on these insights, guiding research questions are formulated for the decade ahead.
{"title":"Supercell Tornadogenesis: Recent Progress in our State of Understanding","authors":"Jannick Fischer, Johannes M. L. Dahl, Brice E. Coffer, Jana Lesak Houser, Paul M. Markowski, Matthew D. Parker, Christopher C. Weiss, Alex Schueth","doi":"10.1175/bams-d-23-0031.1","DOIUrl":"https://doi.org/10.1175/bams-d-23-0031.1","url":null,"abstract":"Abstract Over the last decade, supercell simulations and observations with ever increasing resolution have provided new insights into the vortex-scale processes of tornado formation. This article incorporates these and other recent findings into the existing three-step model by adding an additional fourth stage. The goal is to provide an updated and clear picture of the physical processes occurring during tornadogenesis. Specifically, we emphasize the importance of the low-level wind shear and mesocyclone for tornado potential, the organization and interaction of relatively small-scale pre-tornadic vertical vorticity maxima, and the transition to a tornado-characteristic flow. Based on these insights, guiding research questions are formulated for the decade ahead.","PeriodicalId":9464,"journal":{"name":"Bulletin of the American Meteorological Society","volume":"46 1","pages":""},"PeriodicalIF":8.0,"publicationDate":"2024-04-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140624801","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2024-04-17DOI: 10.1175/bams-d-23-0157.1
John M. Lewis, S. Lakshmivarahan
Abstract A single-day meeting between two theoretical meteorologists took place in 1961 at the Travelers Research Center (TRC) in Hartford, Connecticut. The two scientists were Barry Saltzman and Edward Lorenz, former proteges of V. P. Starr at MIT. Several years before this meeting, Lorenz discovered the following profound result: extended-range weather forecasting was not feasible in the presence of slight errors in initial conditions. The model used was the geostrophic form of a two-level baroclinic model with twelve spectral variables. These results were presented a year earlier at the First Symposium on Numerical Weather Prediction (NWP) in Tokyo, Japan, and met with some skepticism from the NWP elite, dynamical meteorologists, and pioneers in operational NWP. Lorenz held faint hope that Saltzman’s recently developed model of Rayleigh- Bénard convection would produce the profound result found earlier. One of the numerical experiments executed that eventful day with Saltzman’s 7-mode truncated spectral model produced an unexpected result: inability of the model’s 7 variables to settle down and approach a steady state. This occurred when the key parameter, the Rayleigh number, assumed an especially large value, one associated with turbulent convection. And further experimentation with the case delivered the sought-after result that Lorenz had found earlier, and now convincingly found with a simpler model. It built the bridge to chaos theory. The pathway to this exceptional result is explored by revisiting Saltzman’s and Lorenz’s mentorship under V. P. Starr, the authors’ interview with Lorenz in 2002 that complements information in Lorenz’s scientific autobiography, and the authors’ published perspective on Salzman’s 7-mode model.
摘要 1961 年,两位理论气象学家在康涅狄格州哈特福德的旅行者研究中心(TRC)举行了一次为期一天的会议。这两位科学家是巴里-萨尔茨曼(Barry Saltzman)和爱德华-洛伦兹(Edward Lorenz),他们曾是麻省理工学院 V. P. 斯塔尔(V. P. Starr)的门生。在这次会议召开的几年前,洛伦兹发现了以下深刻的结果:在初始条件存在微小误差的情况下,进行大范围天气预报是不可行的。所使用的模型是具有 12 个光谱变量的两级气压模型的地转形式。这些结果是一年前在日本东京举行的第一届数值天气预报(NWP)研讨会上提出的,当时受到了数值天气预报精英、动力学气象学家和实用数值天气预报先驱的怀疑。洛伦兹对萨尔茨曼最近开发的雷利-贝纳德对流模型能产生早先发现的深刻结果抱有微弱的希望。在那个多事的日子里,用萨尔茨曼的 7 模式截断谱模型进行的一次数值实验产生了一个意想不到的结果:模型的 7 个变量无法稳定下来并接近稳定状态。当关键参数雷利数的值特别大(与湍流对流有关)时,就会出现这种情况。进一步的实验证明了洛伦兹早先发现的结果,现在又令人信服地发现了一个更简单的模型。它架起了通向混沌理论的桥梁。通过重温萨尔茨曼和洛伦兹在 V. P. 斯塔尔门下的师徒关系、作者在 2002 年对洛伦兹的访谈(该访谈补充了洛伦兹科学自传中的信息)以及作者发表的关于萨尔茨曼 7 模式模型的观点,我们探索了通往这一非凡结果的道路。
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Pub Date : 2024-04-12DOI: 10.1175/bams-d-23-0087.1
Erik S Krueger, Tyson E Ochsner, B Wade Brorsen
Abstract The USDA Livestock Forage Disaster Program (LFP) offers financial assistance to farmers and ranchers with grazed forage losses caused by fire or drought. Payments for drought losses are based on the United States Drought Monitor (USDM), which is designed to integrate meteorological, agricultural, hydrological, ecological, and socioeconomic drought. Because soil moisture deficit is a more specific measure of agricultural drought, we hypothesized that basing LFP payments on soil moisture observations could better reduce producers’ risk. Therefore, our objectives were to (1) quantify relationships of forage yield with USDM-based LFP payment multipliers and with in situ soil moisture, (2) develop an alternative LFP payment multiplier structure based on in situ soil moisture, and (3) quantify risk reduction using the current and alternative payment structures. We focused on Oklahoma, USA, which has led the nation in LFP payments received and has >25 years of in situ soil moisture observations statewide. Using non-alfalfa hay yield as a surrogate for forage production, we found that LFP payment multiplier values and soil moisture anomaly were each related to yield, and soil moisture anomaly explained 54% of yield variability. However, the USDM-based LFP payment structure sometimes resulted in payments for above average yield, and higher payments did not always correspond with greater yield losses. We developed an alternative soil moisture-based payment structure that reduced financial risk by >20% compared with the current USDM-based structure. Our study identifies an improved LFP payment structure for Oklahoma that can be evaluated and refined in other states or nationwide using other soil moisture data sources.
{"title":"Soil Moisture Information Improves Drought Risk Protection Provided by the USDA Livestock Forage Disaster Program","authors":"Erik S Krueger, Tyson E Ochsner, B Wade Brorsen","doi":"10.1175/bams-d-23-0087.1","DOIUrl":"https://doi.org/10.1175/bams-d-23-0087.1","url":null,"abstract":"Abstract The USDA Livestock Forage Disaster Program (LFP) offers financial assistance to farmers and ranchers with grazed forage losses caused by fire or drought. Payments for drought losses are based on the United States Drought Monitor (USDM), which is designed to integrate meteorological, agricultural, hydrological, ecological, and socioeconomic drought. Because soil moisture deficit is a more specific measure of agricultural drought, we hypothesized that basing LFP payments on soil moisture observations could better reduce producers’ risk. Therefore, our objectives were to (1) quantify relationships of forage yield with USDM-based LFP payment multipliers and with in situ soil moisture, (2) develop an alternative LFP payment multiplier structure based on in situ soil moisture, and (3) quantify risk reduction using the current and alternative payment structures. We focused on Oklahoma, USA, which has led the nation in LFP payments received and has >25 years of in situ soil moisture observations statewide. Using non-alfalfa hay yield as a surrogate for forage production, we found that LFP payment multiplier values and soil moisture anomaly were each related to yield, and soil moisture anomaly explained 54% of yield variability. However, the USDM-based LFP payment structure sometimes resulted in payments for above average yield, and higher payments did not always correspond with greater yield losses. We developed an alternative soil moisture-based payment structure that reduced financial risk by >20% compared with the current USDM-based structure. Our study identifies an improved LFP payment structure for Oklahoma that can be evaluated and refined in other states or nationwide using other soil moisture data sources.","PeriodicalId":9464,"journal":{"name":"Bulletin of the American Meteorological Society","volume":"65 1","pages":""},"PeriodicalIF":8.0,"publicationDate":"2024-04-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140600834","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2024-04-09DOI: 10.1175/bams-d-23-0082.1
William Rudisill, Alan Rhoades, Zexuan Xu, Daniel R. Feldman
Abstract Mountains play an outsized role for water resource availability, and the amount and timing of water they provide depends strongly on temperature. To that end, we ask: how well are atmospheric models capturing mountain temperatures? We synthesize results showing that high resolution, regionally relevant climate models produce two-meter air temperatures (T2m) colder than what is observed (a “cold bias”), particularly in snow-covered mid-latitude mountain ranges during winter. We find common cold biases in 44 studies across global mountain ranges, including single-model and multi-model ensembles. We explore the factors driving these biases and examine the physical mechanisms, data limitations, and observational uncertainties behind T2m. Our analysis suggests that the biases are genuine and not due to observation sparsity or resolution mismatches. Cold biases occur primarily on mountain peaks and ridges, whereas valleys are often warm biased. Our literature review suggests that increasing model resolution does not clearly mitigate the bias. By analyzing data from the SAIL field campaign in the Colorado Rocky Mountains, we test various hypotheses related to cold biases, and find that local wind circulations, longwave radiation, and surface-layer parameterizations contribute to the T2m biases in this particular location. We conclude by emphasizing the value of coordinated model evaluation and development efforts in heavily instrumented mountain locations for addressing the root cause(s) of T2m biases and improving predictive understanding of mountain climates.
{"title":"Are atmospheric models too cold in the mountains? The state of science and insights from the SAIL field campaign","authors":"William Rudisill, Alan Rhoades, Zexuan Xu, Daniel R. Feldman","doi":"10.1175/bams-d-23-0082.1","DOIUrl":"https://doi.org/10.1175/bams-d-23-0082.1","url":null,"abstract":"Abstract Mountains play an outsized role for water resource availability, and the amount and timing of water they provide depends strongly on temperature. To that end, we ask: how well are atmospheric models capturing mountain temperatures? We synthesize results showing that high resolution, regionally relevant climate models produce two-meter air temperatures (T2m) colder than what is observed (a “cold bias”), particularly in snow-covered mid-latitude mountain ranges during winter. We find common cold biases in 44 studies across global mountain ranges, including single-model and multi-model ensembles. We explore the factors driving these biases and examine the physical mechanisms, data limitations, and observational uncertainties behind T2m. Our analysis suggests that the biases are genuine and not due to observation sparsity or resolution mismatches. Cold biases occur primarily on mountain peaks and ridges, whereas valleys are often warm biased. Our literature review suggests that increasing model resolution does not clearly mitigate the bias. By analyzing data from the SAIL field campaign in the Colorado Rocky Mountains, we test various hypotheses related to cold biases, and find that local wind circulations, longwave radiation, and surface-layer parameterizations contribute to the T2m biases in this particular location. We conclude by emphasizing the value of coordinated model evaluation and development efforts in heavily instrumented mountain locations for addressing the root cause(s) of T2m biases and improving predictive understanding of mountain climates.","PeriodicalId":9464,"journal":{"name":"Bulletin of the American Meteorological Society","volume":"300 1","pages":""},"PeriodicalIF":8.0,"publicationDate":"2024-04-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140601215","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2024-04-08DOI: 10.1175/bams-d-24-0082.1
Hans Burchard, Matthew Alford, Manita Chouksey, Giovanni Dematteis, Carsten Eden, Isabelle Giddy, Knut Klingbeil, Arnaud Le Boyer, Dirk Olbers, Julie Pietrzak, Friederike Pollmann, Kurt Polzin, Fabien Roquet, Pablo Sebastia Saez, Sebastiaan Swart, Lars Umlauf, Gunnar Voet, Bethan Wynne-Cattanach
"Linking ocean mixing and overturning circulation" published on 08 Apr 2024 by American Meteorological Society.
美国气象学会于 2024 年 4 月 8 日发表了 "将海洋混合与翻转环流联系起来"。
{"title":"Linking ocean mixing and overturning circulation","authors":"Hans Burchard, Matthew Alford, Manita Chouksey, Giovanni Dematteis, Carsten Eden, Isabelle Giddy, Knut Klingbeil, Arnaud Le Boyer, Dirk Olbers, Julie Pietrzak, Friederike Pollmann, Kurt Polzin, Fabien Roquet, Pablo Sebastia Saez, Sebastiaan Swart, Lars Umlauf, Gunnar Voet, Bethan Wynne-Cattanach","doi":"10.1175/bams-d-24-0082.1","DOIUrl":"https://doi.org/10.1175/bams-d-24-0082.1","url":null,"abstract":"\"Linking ocean mixing and overturning circulation\" published on 08 Apr 2024 by American Meteorological Society.","PeriodicalId":9464,"journal":{"name":"Bulletin of the American Meteorological Society","volume":"115 1","pages":""},"PeriodicalIF":8.0,"publicationDate":"2024-04-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140601346","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2024-04-08DOI: 10.1175/bams-d-23-0055.1
Christopher K. Uejio, Jane Gilbert, Yoonjung Ahn, Ludovica Martella, Leiqiu Hu, Julia Marturano
Abstract Extreme heat contributes to 8,000 to 12,000 excess U.S. deaths per year. Partly due to increasing summer temperatures and a renewed focus on environmental justice, local governments started new initiatives to manage and adapt to extreme heat. For example, Miami-Dade County, Florida, U.S., appointed Jane Gilbert as the world’s first Chief Heat Officer. This manuscript summarizes Miami- Dade County’s preliminary efforts to build local evidence, engage the community, and rapidly respond to extreme heat. The manuscript’s goal is to expedite the translation of existing tools into mainstream extreme heat, health, and equity planning. The study generated local evidence to identify the places and periods of time with elevated heat related illness using a statistical vulnerability and time series analysis, respectively. The places with the highest severe heat-related illness rates had hotter land surface temperatures and/or higher proportions of people who were outdoor workers, indigenous, living in poverty or mobile homes, and households with children. “Everyday” summer conditions instead of rare heatwaves increase the risk of a heat related death. The Chief Heat Officer convened workshops that engaged 298 unique community members on six cross-sectoral heat topics. Key recommendations included: increasing multi-sectoral heat monitoring and risk communication, building more affordable housing, preserving and expanding greenspace, and creating heat resilience hubs. The activities culminated in a Heat Action Plan, which was completed in less than two years from the receipt of project funding.
{"title":"Rapidly Developing a Community and Evidence Based Heat Action Plan","authors":"Christopher K. Uejio, Jane Gilbert, Yoonjung Ahn, Ludovica Martella, Leiqiu Hu, Julia Marturano","doi":"10.1175/bams-d-23-0055.1","DOIUrl":"https://doi.org/10.1175/bams-d-23-0055.1","url":null,"abstract":"Abstract Extreme heat contributes to 8,000 to 12,000 excess U.S. deaths per year. Partly due to increasing summer temperatures and a renewed focus on environmental justice, local governments started new initiatives to manage and adapt to extreme heat. For example, Miami-Dade County, Florida, U.S., appointed Jane Gilbert as the world’s first Chief Heat Officer. This manuscript summarizes Miami- Dade County’s preliminary efforts to build local evidence, engage the community, and rapidly respond to extreme heat. The manuscript’s goal is to expedite the translation of existing tools into mainstream extreme heat, health, and equity planning. The study generated local evidence to identify the places and periods of time with elevated heat related illness using a statistical vulnerability and time series analysis, respectively. The places with the highest severe heat-related illness rates had hotter land surface temperatures and/or higher proportions of people who were outdoor workers, indigenous, living in poverty or mobile homes, and households with children. “Everyday” summer conditions instead of rare heatwaves increase the risk of a heat related death. The Chief Heat Officer convened workshops that engaged 298 unique community members on six cross-sectoral heat topics. Key recommendations included: increasing multi-sectoral heat monitoring and risk communication, building more affordable housing, preserving and expanding greenspace, and creating heat resilience hubs. The activities culminated in a Heat Action Plan, which was completed in less than two years from the receipt of project funding.","PeriodicalId":9464,"journal":{"name":"Bulletin of the American Meteorological Society","volume":"22 1","pages":""},"PeriodicalIF":8.0,"publicationDate":"2024-04-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140600830","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}