Articles | Volume 28, issue 4
https://doi.org/10.5194/npg-28-615-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/npg-28-615-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Reduced non-Gaussianity by 30 s rapid update in convective-scale numerical weather prediction
RIKEN Center for Computational Science, Kobe, Japan
Center for Oceanic and Atmospheric Research (CIMA-UBA/CONICET); Atmospheric and Oceanographic Science Department, FCEyN, University of Buenos Aires; French-Argentinean Institute for the Study of Climate and its Impacts (UMI-IFAECI/CNRS-CONICET-UBA), Buenos Aires, Argentina
Guo-Yuan Lien
Research and Development Center, Central Weather Bureau, Taipei, Taiwan
Keiichi Kondo
Department of Observation and Data Assimilation Research, Meteorological Research Institute, Tsukuba, Japan
Shigenori Otsuka
RIKEN Center for Computational Science, Kobe, Japan
RIKEN Cluster for Pioneering Research, Kobe, Japan
RIKEN Interdisciplinary Theoretical and Mathematical Sciences Program, Kobe, Japan
Takemasa Miyoshi
CORRESPONDING AUTHOR
RIKEN Center for Computational Science, Kobe, Japan
RIKEN Cluster for Pioneering Research, Kobe, Japan
RIKEN Interdisciplinary Theoretical and Mathematical Sciences Program, Kobe, Japan
Atmospheric and Oceanic Science Department, University of Maryland, College Park, Maryland, USA
Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan
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Subject: Predictability, probabilistic forecasts, data assimilation, inverse problems | Topic: Climate, atmosphere, ocean, hydrology, cryosphere, biosphere | Techniques: Simulation
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In Earth science, data assimilation plays an important role in integrating real-world observations with numerical simulations for improving subsequent predictions. To overcome the time-consuming computations of conventional data assimilation methods, this paper proposes using quantum annealing machines. Using the D-Wave quantum annealer, the proposed method found solutions with comparable accuracy to conventional approaches and significantly reduced computational time.
Vivian A. Montiforte, Hans E. Ngodock, and Innocent Souopgui
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Kenta Kurosawa, Shunji Kotsuki, and Takemasa Miyoshi
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Dikraa Khedhaouiria, Stéphane Bélair, Vincent Fortin, Guy Roy, and Franck Lespinas
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Nonlin. Processes Geophys., 29, 133–139, https://doi.org/10.5194/npg-29-133-2022, https://doi.org/10.5194/npg-29-133-2022, 2022
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Zhao Liu, Shaoqing Zhang, Yang Shen, Yuping Guan, and Xiong Deng
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Sangeetika Ruchi, Svetlana Dubinkina, and Jana de Wiljes
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To infer information of an unknown quantity that helps to understand an associated system better and to predict future outcomes, observations and a physical model that connects the data points to the unknown parameter are typically used as information sources. Yet this problem is often very challenging due to the fact that the unknown is generally high dimensional, the data are sparse and the model can be non-linear. We propose a novel approach to address these challenges.
Michiel Van Ginderachter, Daan Degrauwe, Stéphane Vannitsem, and Piet Termonia
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A generic methodology is developed to estimate the model error and simulate the model uncertainty related to a specific physical process. The method estimates the model error by comparing two different representations of the physical process in otherwise identical models. The found model error can then be used to perturb the model and simulate the model uncertainty. When applying this methodology to deep convection an improvement in the probabilistic skill of the ensemble forecast is found.
Valentin Resseguier, Wei Pan, and Baylor Fox-Kemper
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Geophysical flows span a broader range of temporal and spatial scales than can be resolved numerically. One way to alleviate the ensuing numerical errors is to combine simulations with measurements, taking account of the accuracies of these two sources of information. Here we quantify the distribution of numerical simulation errors without relying on high-resolution numerical simulations. Specifically, small-scale random vortices are added to simulations while conserving energy or circulation.
Sebastian Scher and Gabriele Messori
Nonlin. Processes Geophys., 26, 381–399, https://doi.org/10.5194/npg-26-381-2019, https://doi.org/10.5194/npg-26-381-2019, 2019
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Neural networks are a technique that is widely used to predict the time evolution of physical systems. For this the past evolution of the system is shown to the neural network – it is
trained– and then can be used to predict the evolution in the future. We show some limitations in this approach for certain systems that are important to consider when using neural networks for climate- and weather-related applications.
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Short summary
Effective use of observations with numerical weather prediction models, also known as data assimilation, is a key part of weather forecasting systems. For precise prediction at the scales of thunderstorms, fast nonlinear processes pose a grand challenge because most data assimilation systems are based on linear processes and normal distribution errors. We investigate how, every 30 s, weather radar observations can help reduce the effect of nonlinear processes and nonnormal distributions.
Effective use of observations with numerical weather prediction models, also known as data...