用生成模型预测城市地表不透水层变化,效果优于不做预测的基线。
Geospatial Diffusion for Land Cover Imperviousness Change Forecasting
- 将土地覆盖变化视为生成任务,用扩散模型学习历史数据中的时空模式。
- 在12个大都市区测试中,0.7km²以上分辨率下平均误差低于零变化基线。
- 适合关注城市化影响、气候风险评估的研究者使用。
土地覆盖现状及未来变化对地球系统过程有重要影响。例如,不透水地表会升温、加速地表径流并减少地下水渗透,进而影响区域水文与洪涝风险。尽管地球系统模型在高分辨率下对水文和大气过程的未来预测能力不断提升,但对土地利用与土地覆盖变化(LULC)的预测仍相对滞后,而后者是风险评估的关键输入。本文提出一种新范式,利用生成式人工智能(GenAI)进行土地覆盖变化预测,将LULC预测视为基于历史和辅助数据的数据合成问题。我们讨论了生成模型应具备的特性,并通过全美历史数据验证方法可行性。具体而言,训练了一个用于十年尺度不透水层预测的扩散模型,并与假设无变化的基线进行比较。在12个大都市区、训练时留出一年数据的评估中,当平均分辨率≥0.7×0.7 km²时,该模型的平均绝对误差(MAE)低于基线。结果表明,此类生成模型能有效捕捉历史数据中对预测未来变化具有重要意义的时空模式。最后,我们展望未来研究方向:融入地球物理属性等辅助信息,并通过驱动变量支持多情景模拟。
原文摘要 · Abstract (English)
Land cover, both present and future, has a significant effect on several important Earth system processes. For example, impervious surfaces heat up and speed up surface water runoff and reduce groundwater infiltration, with concomitant effects on regional hydrology and flood risk. While regional Earth System models have increasing skill at forecasting hydrologic and atmospheric processes at high resolution in future climate scenarios, our ability to forecast land-use and land-cover change (LULC), a critical input to risk and consequences assessment for these scenarios, has lagged behind. In this paper, we propose a new paradigm exploiting Generative AI (GenAI) for land cover change forecasting by framing LULC forecasting as a data synthesis problem conditioned on historical and auxiliary data-sources. We discuss desirable properties of generative models that fundament our research premise, and demonstrate the feasibility of our methodology through experiments on imperviousness forecasting using historical data covering the entire conterminous United States. Specifically, we train a diffusion model for decadal forecasting of imperviousness and compare its performance to a baseline that assumes no change at all. Evaluation across 12 metropolitan areas for a year held-out during training indicate that for average resolutions $\geq 0.7\times0.7km^2$ our model yields MAE lower than such a baseline. This finding corroborates that such a generative model can capture spatiotemporal patterns from historical data that are significant for projecting future change. Finally, we discuss future research to incorporate auxiliary information on physical properties about the Earth, as well as supporting simulation of different scenarios by means of driver variables.
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