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  • 1
    Keywords: Weather forecasting. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (588 pages)
    Edition: 1st ed.
    ISBN: 9780128117156
    DDC: 551.63
    Language: English
    Note: Front Cover -- Sub-seasonal to Seasonal Prediction: The Gap Between Weather and Climate Forecasting -- Copyright -- Contents -- Contributors -- Preface -- Acknowledgements -- Part I: Setting the Scene -- Chapter 1: Introduction: Why Sub-seasonal to Seasonal Prediction (S2S)? -- 1. History of Numerical Weather and Climate Forecasting -- 2. Sub-seasonal to Seasonal Forecasting -- 2.1. The Discovery of Sources of Sub-seasonal to Seasonal Predictability Associated With Atmosphere, Ocean, and Land Proc ... -- 2.2. Improvements in Numerical Weather Forecasting -- 2.3. Development of Seamless Prediction -- 2.4. Demand From Users for S2S Forecasts -- 3. Recent National and International Efforts on Sub-seasonal to Seasonal Prediction -- 4. Structure of This Book -- Chapter 2: Weather Forecasting: What Sets the Forecast Skill Horizon? -- 1. Introduction -- 2. The Basics of Numerical Weather Prediction -- 2.1. The Atmosphere as a Dynamical System -- 2.2. Predictability -- 2.3. Scale-Dependent Behavior -- 2.4. Coupled Systems -- 3. The Evolution of NWP Techniques -- 3.1. Computational Infrastructure -- 3.2. Observing Systems -- 3.3. Data Assimilation -- 3.4. Modeling -- 3.5. Improvements in Forecast Performance -- 3.6. Weather Versus Climate Prediction -- 4. Enhancement of Predictable Signals -- 4.1. Spatiotemporal Aggregation -- 4.2. Ensemble Averaging -- 4.3. Removal of Systematic Errors -- 5. Ensemble Techniques: Brief Introduction -- 5.1. Background -- 5.2. Methodology -- 5.3. Use of Ensembles -- 6. Expanding the Forecast Skill Horizon -- 7. Concluding Remarks: Lessons for S2S Forecasting -- Acknowledgments -- Chapter 3: Weather Within Climate: Sub-seasonal Predictability of Tropical Daily Rainfall Characteristics -- 1. Introduction -- 2. Data and Methods -- 2.1. Daily Rainfall and OLR -- 2.2. S2S Forecasts. , 2.3. Method to Estimate the Spatial Coherence -- 3. Results -- 3.1. Daily Rainfall Characteristics of the Indian Summer Monsoon -- 3.2. Sub-seasonal Modulation of Spatial Coherence Across India -- 3.3. Sub-seasonal Modulation of Spatial Coherence Over the Whole Tropical Zone -- 3.4. Skill and Spatial Coherence of S2S Reforecasts -- 4. Discussion and Concluding Remarks -- Chapter 4: Identifying Wave Processes Associated With Predictability Across Time Scales: An Empirical Normal Mode Approach -- 1. Introduction -- 2. Partitioning Atmospheric Behavior Using Its Conservation Properties -- 2.1. Partitioning Variability: Background State and Wave Activity -- 2.2. Wave Activity Conservation Laws -- 2.3. The Implications of Wave-Activity Conservation for Modes of Variability -- 3. The ENM Approach to Observed Data and Models and Its Relevance to S2S Dynamics and Predictability -- 3.1. ENMs: Bridging Principal Component, Normal Modes, and Conservation Laws -- 3.2. ENM in Applications Relevant to Predictability Across Time Scales -- 3.3. ENM Application to the Atmospheric S2S Variability -- 4. Conclusion -- Acknowledgments -- Part II: Sources of S2S Predictability -- Chapter 5: The Madden-Julian Oscillation -- 1. Introduction -- 2. The Real-Time Multivariate MJO Index -- 3. Observed MJO Structure -- 4. The Relationship Between the MJO and Tropical and Extratropical Weather -- 5. Theories and Mechanisms for MJO Initiation, Maintenance, and Propagation -- 6. The Representation of the MJO in Weather and Climate Models -- 7. MJO Prediction -- 7.1. Sub-seasonal and Interannual Variations in Forecast Skill -- 8. Future Priorities for MJO Research for S2S Prediction -- 8.1. Linking Theory and Modeling -- 8.2. MJO Initiation -- 8.3. Predicting the Impacts of the MJO -- Acknowledgments. , Chapter 6: Extratropical Sub-seasonal to Seasonal Oscillations and Multiple Regimes: The Dynamical Systems View -- 1. Introduction and Motivation -- 2. Multiple Midlatitude Regimes and Low-Frequency Oscillations -- 2.1. The Case for Multiple Regimes and Their Classification -- 2.2. Theoretical Basis of Multiple Regimes -- Rossby Wave Propagation and Interference -- 3. Extratropical Oscillations in the S2S Band -- 3.1. Phenomenological Description -- Variations of Geopotential Height -- Oscillatory Features in Time and Space -- 3.2. Topographic Instability and Hopf Bifurcation -- 4. Low-Order, Data-Driven Modeling, Dynamical Analysis, and Prediction -- 4.1. Background and Methodological LOM Developments -- 4.2. Dynamical Diagnostics and Empirical Prediction on S2S Scales -- 4.3. LFV and Multilayer Stochastic Closure: A Simple Illustration -- 5. Concluding Remarks -- Acknowledgments -- Chapter 7: Tropical-Extratropical Interactions and Teleconnections -- 1. Introduction -- 2. Tropical Influence on the Extratropical Atmosphere -- 2.1. Observed MJO Influences -- 2.2. Extratropical Atmospheric Response to Tropical Thermal Forcing -- 3. Extratropical Influence on the Tropics -- 3.1. Extratropical Influences on Tropical Convection and the MJO -- 3.2. Diagnosing Intraseasonal Extratropical Influences on the Tropics -- 4. Tropical-Extratropical, Two-Way Interactions -- 4.1. Forcing of Extratropical Waves Through Two-Way Interactions -- 4.2. Three-Dimensional Instability Theory -- 5. Summary and Discussion -- Appendix. Technical Matters Relating to Section 4.2 -- Chapter 8: Land Surface Processes Relevant to Sub-seasonal to Seasonal (S2S) Prediction -- 1. Introduction -- 2. Process of Land-Atmosphere Interaction -- 2.1. Surface Fluxes -- 2.2. Land-Surface States -- 2.3. Boundary Layer (BL) Response -- 2.4. Timescales. , 3. A Brief History of Land-Surface Models -- 3.1. Origin and Evolution of Land-Surface Models -- 3.2. LSMs at Operational Forecast Centers -- 3.3. LSM Initialization and Data Assimilation -- 4. Predictability and Prediction -- 5. Improving Land-Driven Prediction -- 5.1. Validation -- 5.2. Initialization -- 5.3. Unconsidered Elements -- 5.4. Coupled Land-Atmosphere Model Development -- Chapter 9: Midlatitude Mesoscale Ocean-Atmosphere Interaction and Its Relevance to S2S Prediction -- 1. Introduction -- 2. Data and Models -- 2.1. Uncoupled Integrations -- 2.2. Coupled Integrations -- 3. Mesoscale Ocean-Atmosphere Interaction in the Atmospheric Boundary Layer -- 4. Local Tropospheric Response -- 5. Remote Tropospheric Response -- 6. Impact on Ocean Circulation -- 7. Implications for S2S Prediction -- 8. Summary and Conclusions -- Acknowledgments -- Chapter 10: The Role of Sea Ice in Sub-seasonal Predictability -- 1. Introduction -- 2. Sea Ice in the Coupled Atmosphere-Ocean System -- 2.1. Sea Ice Physics -- 2.2. Sea Ice Observations -- 2.3. Sea Ice in Models and Reanalyses -- 3. Sea Ice Distribution, Seasonality, and Variability -- 4. Sources of Sea Ice Predictability at the Sub-seasonal to Seasonal Timescale -- 4.1. Persistence -- 4.2. Other Mechanisms -- 5. Sea Ice Sub-seasonal to Seasonal Predictability and Prediction Skill in Models -- 5.1. Potential Sea Ice Predictability -- 5.2. Skill of Sea Ice Prediction Systems at Sub-seasonal Timescales -- 5.2.1. Short-Term Predictions -- 5.2.2. Sub-seasonal to Seasonal Predictions -- 6. Impact of Sea Ice on Sub-seasonal Predictability -- 6.1. Impacts in the Polar Regions -- 6.2. Impacts Outside Polar Regions -- 7. Concluding Remarks -- Acknowledgments -- Chapter 11: Sub-seasonal Predictability and the Stratosphere -- 1. Introduction -- 2. Stratosphere-Troposphere Coupling in the Tropics. , 2.1. How Does the QBO Influence the Tropical Troposphere? -- 2.2. Predictability Related to Tropical Stratosphere-Troposphere Coupling -- 3. Stratosphere-Troposphere Coupling in the Extratropics -- 3.1. An Overview of Polar Vortex Variability -- 3.2. What Drives Polar Vortex Variability? -- 3.3. How Does Stratospheric Polar Vortex Variability Influence Surface Climate? -- 3.4. Other Manifestations of Extratropical Stratosphere-Troposphere Coupling -- 4. Predictability Related to Extratropical Stratosphere-Troposphere Coupling -- 4.1. How Accurately Can the Polar Stratosphere be Predicted? -- 4.2. S2S Extratropical Forecast Skill Associated With Strong and Weak Polar Vortex Events -- 4.3. S2S Extratropical Forecast Skill Associated With Stratosphere-Troposphere Pathways -- 5. Summary and Outlook -- 5.1. What Determines How Well a Model Represents Stratosphere-Troposphere Coupling? -- 5.1.1. Role of Model Lid Height and Vertical Resolution -- 5.1.2. Influence of the Tropospheric State and Biases -- 5.1.3. Influence of Different Drivers on Stratosphere-Troposphere Coupling Efficacy -- 5.2. How Can We Use Sub-seasonal Prediction Data in New Ways to Study Stratospheric Dynamics and Stratosphere-Troposphere ... -- Part III: S2S Modeling and Forecasting -- Chapter 12: Forecast System Design, Configuration, and Complexity -- 1. Introduction -- 2. Requirements and Constraints of the Operational Sub-seasonal Forecast -- 3. Effect of Ensemble Size and Lagged Ensemble -- 3.1. Effect of Ensemble Size -- 3.2. Uncertainty of Skill Estimate -- 3.3. Effect of LAF Ensemble -- 4. Real-Time Forecast Configuration -- 5. Reforecast Configuration -- 6. Summary and Concluding Remarks -- Acknowledgments -- Chapter 13: Ensemble Generation: The TIGGE and S2S Ensembles -- 1. Global Sub-seasonal and Seasonal Prediction Is an Initial Value Problem. , 2. Ensembles Provide More Complete and Valuable Information Than Single States.
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  • 2
    Publication Date: 2023-02-08
    Description: Weather and climate variations on subseasonal to decadal time scales can have enormous social, economic, and environmental impacts, making skillful predictions on these time scales a valuable tool for decision-makers. As such, there is a growing interest in the scientific, operational, and applications communities in developing forecasts to improve our foreknowledge of extreme events. On subseasonal to seasonal (S2S) time scales, these include high-impact meteorological events such as tropical cyclones, extratropical storms, floods, droughts, and heat and cold waves. On seasonal to decadal (S2D) time scales, while the focus broadly remains similar (e.g., on precipitation, surface and upper-ocean temperatures, and their effects on the probabilities of high-impact meteorological events), understanding the roles of internal variability and externally forced variability such as anthropogenic warming in forecasts also becomes important. The S2S and S2D communities share common scientific and technical challenges. These include forecast initialization and ensemble generation; initialization shock and drift; understanding the onset of model systematic errors; bias correction, calibration, and forecast quality assessment; model resolution; atmosphere-ocean coupling; sources and expectations for predictability; and linking research, operational forecasting, and end-user needs. In September 2018 a coordinated pair of international conferences, framed by the above challenges, was organized jointly by the World Climate Research Programme (WCRP) and the World Weather Research Programme (WWRP). These conferences surveyed the state of S2S and S2D prediction, ongoing research, and future needs, providing an ideal basis for synthesizing current and emerging developments in these areas that promise to enhance future operational services. This article provides such a synthesis.
    Type: Article , PeerReviewed
    Format: text
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  • 3
    Publication Date: 2021-05-12
    Description: Producing probabilistic subseasonal forecasts of extreme events up to six weeks in advance is crucial for many economic sectors. In agribusiness, this time scale is particularly critical because it allows for mitigation strategies to be adopted for counteracting weather hazards and taking advantage of opportunities. For example, spring frosts are detrimental for many nut trees, resulting in dramatic losses at harvest time. To explore subseasonal forecast quality in boreal spring, identified as one of the most sensitive times of the year by agribusiness end users, we build a multisystem ensemble using four models involved in the Subseasonal to Seasonal Prediction project (S2S). Two-meter temperature forecasts are used to analyze cold spell predictions in the coastal Black Sea region, an area that is a global leader in the production of hazelnuts. When analyzed at the global scale, the multisystem ensemble probabilistic forecasts for near-surface temperature are better than climatological values for several regions, especially the tropics, even many weeks in advance; however, in the coastal Black Sea, skill is low after the second forecast week. When cold spells are predicted instead of near-surface temperatures, skill improves for the region, and the forecasts prove to contain potentially useful information to stakeholders willing to put mitigation plans into effect. Using a cost–loss model approach for the first time in this context, we show that there is added value of having such a forecast system instead of a business-as-usual strategy, not only for predictions released 1–2 weeks ahead of the extreme event, but also at longer lead times.
    Description: Published
    Description: 237–254
    Description: 4A. Oceanografia e clima
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 4
    Publication Date: 2022-10-26
    Description: © The Author(s), 2019. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Subramanian, A. C., Balmaseda, M. A., Centurioni, L., Chattopadhyay, R., Cornuelle, B. D., DeMott, C., Flatau, M., Fujii, Y., Giglio, D., Gille, S. T., Hamill, T. M., Hendon, H., Hoteit, I., Kumar, A., Lee, J., Lucas, A. J., Mahadevan, A., Matsueda, M., Nam, S., Paturi, S., Penny, S. G., Rydbeck, A., Sun, R., Takaya, Y., Tandon, A., Todd, R. E., Vitart, F., Yuan, D., & Zhang, C. Ocean observations to improve our understanding, modeling, and forecasting of subseasonal-to-seasonal variability. Frontiers in Marine Science, 6, (2019): 427, doi:10.3389/fmars.2019.00427.
    Description: Subseasonal-to-seasonal (S2S) forecasts have the potential to provide advance information about weather and climate events. The high heat capacity of water means that the subsurface ocean stores and re-releases heat (and other properties) and is an important source of information for S2S forecasts. However, the subsurface ocean is challenging to observe, because it cannot be measured by satellite. Subsurface ocean observing systems relevant for understanding, modeling, and forecasting on S2S timescales will continue to evolve with the improvement in technological capabilities. The community must focus on designing and implementing low-cost, high-value surface and subsurface ocean observations, and developing forecasting system capable of extracting their observation potential in forecast applications. S2S forecasts will benefit significantly from higher spatio-temporal resolution data in regions that are sources of predictability on these timescales (coastal, tropical, and polar regions). While ENSO has been a driving force for the design of the current observing system, the subseasonal time scales present new observational requirements. Advanced observation technologies such as autonomous surface and subsurface profiling devices as well as satellites that observe the ocean-atmosphere interface simultaneously can lead to breakthroughs in coupled data assimilation (CDA) and coupled initialization for S2S forecasts. These observational platforms should also be tested and evaluated in ocean observation sensitivity experiments with current and future generation CDA and S2S prediction systems. Investments in the new ocean observations as well as model and DA system developments can lead to substantial returns on cost savings from disaster mitigation as well as socio–economic decisions that use S2S forecast information.
    Description: AS was funded by NOAA Climate Variability and Prediction Program (NA14OAR4310276) and the NSF Earth System Modeling Program (OCE1419306). CD was funded by NA16OAR4310094. SG and DG were funded by NASA awards NNX14AO78G and 80NSSC19K0059. DY was supported by NSFC (91858204, 41720104008, and 41421005).
    Keywords: Subseasonal ; Seasonal ; Predictions ; Air-sea interaction ; Satellite ; Argo ; Gliders ; Drifters
    Repository Name: Woods Hole Open Access Server
    Type: Article
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