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Ensemble downscaling in coupled solar wind-magnetosphere modeling for space weather forecasting

机译:集成的按比例缩小的太阳风-磁层耦合模型用于空间天气预报

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摘要

Advanced forecasting of space weather requires simulation of the whole Sun-to-Earth system, which necessitates driving magnetospheric models with the outputs from solar wind models. This presents a fundamental difficulty, as the magnetosphere is sensitive to both large-scale solar wind structures, which can be captured by solar wind models, and small-scale solar wind “noise,” which is far below typical solar wind model resolution and results primarily from stochastic processes. Following similar approaches in terrestrial climate modeling, we propose statistical “downscaling” of solar wind model results prior to their use as input to a magnetospheric model. As magnetospheric response can be highly nonlinear, this is preferable to downscaling the results of magnetospheric modeling. To demonstrate the benefit of this approach, we first approximate solar wind model output by smoothing solar wind observations with an 8 h filter, then add small-scale structure back in through the addition of random noise with the observed spectral characteristics. Here we use a very simple parameterization of noise based upon the observed probability distribution functions of solar wind parameters, but more sophisticated methods will be developed in the future. An ensemble of results from the simple downscaling scheme are tested using a model-independent method and shown to add value to the magnetospheric forecast, both improving the best estimate and quantifying the uncertainty. We suggest a number of features desirable in an operational solar wind downscaling scheme.Key Points class="unordered" style="list-style-type:disc">Solar wind models must be downscaled in order to drive magnetospheric models Ensemble downscaling is more effective than deterministic downscaling The magnetosphere responds nonlinearly to small-scale solar wind fluctuations
机译:先进的空间天气预测需要对整个太阳到地球系统进行仿真,这需要使用太阳风模型的输出来驱动磁层模型。由于磁层对大型太阳风结构(可由太阳风模型捕获)和小规模太阳风“噪声”(都远低于典型的太阳风模型分辨率和结果)敏感,因此这是一个基本难题。主要来自随机过程。遵循类似的地面气候建模方法,我们建议在将太阳风模型结果用作磁层模型的输入之前,对其进行统计“缩减”。由于磁层响应可能是高度非线性的,因此这比缩小磁层建模的结果更好。为了证明这种方法的好处,我们首先通过使用8 h滤波器对太阳风观测值进行平滑处理来近似太阳风模型输出,然​​后通过添加具有观察到的光谱特征的随机噪声来添加小规模结构。在这里,我们基于观测到的太阳风参数的概率分布函数,使用了非常简单的噪声参数化方法,但是将来会开发出更复杂的方法。使用与模型无关的方法对简单缩减方案的结果进行了测试,结果表明该结果可为磁层预测增加价值,既可以改善最佳估计值,又可以量化不确定性。我们建议在运行中的太阳风缩减方案中需要一些功能。要点 class =“ unordered” style =“ list-style-type:disc”> <!-list-behavior = unordered prefix-word = mark -type = disc max-label-size = 0-> 必须缩减太阳能风模型以驱动磁层模型 集合缩减比确定性缩减更有效
  • 磁层对小规模太阳风起伏非线性响应
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