Collaborative Research: North American Warm-season Extremes in a Changing Climate: Large-scale Drivers and Local Feedbacks

在美国大部分地区，气候变化将主要通过其对暖季极端事件（如洪水、热浪、火灾和干旱）的影响而感受到。 基本热力学表明，这些事件的严重性和频率应该增加，例如，在气候变暖的情况下，最热的热浪可能会变得更热，风暴强度可能会增加，因为温暖的空气含有更多的水分。 热力学的论点有所帮助，但影响极端事件的全套过程是广泛的，涉及广泛的空间尺度，从数公里尺度的雷暴到驱动天气系统的半球尺度的急流。 广泛的尺度范围使使用天气和气候模型研究极端事件变化的努力变得复杂，因为在全球变暖的数十年发展过程中，在所有相关空间尺度上模拟所有相关过程的蛮力努力即使在最大的计算机上也是不切实际的。 气候模式可以模拟数十年甚至数百年的全球气候系统，但分辨率太粗糙（网格间距可能为100公里），无法代表强烈风暴的尺度。 特别是，它们没有捕捉到中尺度对流系统（MCS），而这些系统是美国大陆大部分恶劣天气的原因。 另一种称为伪全球变暖（PGW）的方法使用高分辨率模型来模拟观测到的极端事件，并通过修改环境条件来重复模拟，以代表更温暖的气候。 PGW模拟非常有价值，但它们只允许考虑气候变化如何影响特定事件的严重性，因此无法研究极端事件发生频率的变化。 此外，PGW模拟通常使用区域模式进行，因此不能正确反映半球尺度大气环流变化的影响。本项目开发了一种方法，用于研究气候变暖中的极端事件变化，解决多尺度问题，并可以检查极端事件频率和其他汇总统计数据。 首先，一个高分辨率的全球模式，跨尺度预测模式（MPAS）被用来模拟过去30年（1990年至2019年）的天气和气候。 网格间距为15公里的模式是能够代表MCS。 第二，在这一“自然运行”中确定极端事件，并对海洋表面温度和其他表面条件进行修改，以代表未来的变暖。 这些修改是使用耦合模式相互比较项目（CMIP）的气候模式模拟产生的。 的resimulations是一种形式的PGW只有一个全球域，使强度的变化可以检查占整个范围的空间尺度。 第三，一组30个温暖的季节（5月至11月）MPAS模拟使用CMIP模式输出，以代表未来的气候变化。 暖季模拟遵循PGW方法，但整个季节持续时间意味着模拟不遵循特定事件，而是显示极端事件的典型季节如何因温暖条件而变化。 这些模拟要解决的一个问题是北美上空急流变化对洪水和热浪的影响，因为气候模型通常显示喷气式飞机的减少，水平风速在美国大陆的速度增加的北部和南部。这项工作是社会以及科学的兴趣，考虑到极端事件的破坏性影响和价值的更好的信息极端事件的变化，指导决策。 该项目还为五名研究生和一名本科生研究助理提供支助和培训。 该项目生成的模拟结果可供研究界使用，缩小版的输出结果被托管在一个计算机中心上，以便参与该项目的大学研究人员通过计算机笔记本查阅。 外展是通过初级馆长计划北卡罗来纳州自然科学博物馆（NCMNS），对现场生物学和保护感兴趣的高中学生的计划进行。 学生们收集当地天气事件及其影响的实地测量结果，包括昆虫爆发、霉菌、洪水和暴雨的其他后果。 活动指南是根据这些活动创建的，并通过全国地球科学教师协会传播。该奖项反映了NSF的法定使命，并通过使用基金会的知识价值和更广泛的影响审查标准进行评估，被认为值得支持。

Throughout much of the US climate change will be felt largely through its effects on warm season extreme events like flooding rains, heat waves, fires, and droughts. Basic thermodynamics suggests that the severity and frequency of these events should increase, for instance the hottest heat waves are likely to get hotter in a warming climate and storm intensity is likely to increase because warmer air holds more moisture. The thermodynamic arguments help but the full suite of processes that affect extreme events is extensive and involves a broad range of spatial scales, from the multi-kilometer scale of thunderstorms to the hemispheric scale of the jet streams that drive weather systems. The broad scale range complicates efforts to study extreme event change using weather and climate models, as a brute force effort to simulate all the relevant processes at all the relevant spatial scales, occurring over the decades-long progression of global warming, is not practical even on the largest computers. Climate models can simulate the full global climate system for decades and even centuries but at resolutions too coarse (perhaps 100km grid spacing) to represent the scales of intense storms. In particular they do not capture the mesoscale convective systems (MCSs) which account for much of the severe weather over the continental US. An alternative approach called pseudo-global warming (PGW) uses a high-resolution model to simulate an observed extreme event, and the simulation is repeated with modifications to the ambient conditions to represent the warmer climate. PGW simulations are quite valuable but they only allow consideration of how climate change affects the severity of specific events, thus they do not enable research on changes in the frequency of occurrence of extreme events. Also, PGW simulations are typically conducted using regional models and thus do not properly represent the effects of changes in the hemispheric-scale atmospheric circulation.This project develops a methodology for looking at extreme event change in a warming climate which addresses the multi-scale issue and enables examination of extreme event frequency and other aggregate statistics. First, a high-resolution global model, the Model for Prediction Across Scales (MPAS) is used to simulate the weather and climate of the past 30 years (1990 to 2019). With a grid spacing of 15km the model is capable of representing MCSs. Second, extreme events are identified in this "nature run" and resimulated with modifications to sea surface temperatures and other surface conditions to represent future warming. The modifications are generated using climate model simulations from the Coupled Model Intercomparison Project (CMIP). The resimulations are a form of PGW only with a global domain, so that changes in intensity can be examined accounting for the full range of spatial scales. Third, a set of 30 warm season (May to November) MPAS simulations using CMIP model output is generated to represent future climate change. The warm season simulations follow the PGW approach but the full season duration means that the simulations do not follow particular events but instead show how a typical season of extreme events changes due to warmer conditions. One issue to be addressed with these simulations is the effect of changes in the jet streams over North America on floods and heat waves, as climate models typically show a reduction in jet-level wind speed over the continental US with increases in speed to the north and south.The work is of societal as well as scientific interest given the damaging effects of extreme events and the value of better information on extreme event change to guide decision making. The project also provides support and training to five graduate students and an undergraduate research assistant. Simulations generated in the project are made available to the research community, and reduced versions of the output are hosted on a JupyterHub to provide access to researchers at the universities participating in the project through Jupyter Notebooks. Outreach is conducted through the Junior Curator program North Carolina Museum of Natural Sciences (NCMNS), a program for high school students interested in field biology and conservation. The students collect field mesaurements of local weather events and their impacts, including insect outbreaks, mold, flooding, and other after-effects of heavy rain. Activity guides are created based on these activities and disseminated through the National Association of Geoscience Teachers.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.