Earth and Environmental Sciences, The City University of New York - Graduate Center, New York, USA.
Department of Earth and Atmospheric Science, The City University of New York - City College, New York, USA.
Sci Rep. 2024 Nov 14;14(1):27947. doi: 10.1038/s41598-024-78704-9.
The remnants of Hurricane Ida caused major damage and death in the United States on September 1st, 2021, and 11 people drowned in flooded basement apartments within New York City (NYC). It was catastrophic because the maximum hourly precipitation intensity, recorded as 3.47 inches (88.1 mm) per hour at Central Park, was unprecedentedly high for the NYC region. The stormwater infrastructure in NYC is built for 1.75 inches (44.5 mm) per hour, and so understanding the dynamic risk associated with Ida can inform city planning efforts for climate change's impact on short duration extreme precipitation events. We contextualize this storm's record-breaking hourly intensity within the historical record as well as project its risk in the near- to medium-term future using nonstationary stochastic models. These models are conditioned on average temperature (T) and cooling degree day (CDD) projections from three climate models as a covariate, each with a SSP 126 and SSP 370 scenario. The likelihood of such a storm was slowly increasing even before Ida happened, but the projected aggregate reoccurrence risk of an event of Ida's magnitude over time from the non-stationary models ranges from 4 to 52 times higher than the risk given by the stationary model. Using CDD as a covariate resulted in risks that were more than twice the magnitude than when using T. Presenting both covariates provides a broader envelope of uncertainty, which highlights the importance and nuances in the choice of a regionally appropriate covariate for non-stationary risk analysis.
2021 年 9 月 1 日,飓风“艾达”在美国造成了重大破坏和人员死亡,纽约市(NYC)有 11 人淹死在被洪水淹没的地下室公寓里。这场风暴之所以具有灾难性,是因为中央公园每小时记录到的最大降水强度为 3.47 英寸(88.1 毫米),这是纽约地区前所未有的高值。纽约市的雨水基础设施是按照每小时 1.75 英寸(44.5 毫米)的标准建造的,因此,了解与“艾达”相关的动态风险可以为城市规划工作提供信息,以应对气候变化对短时间极端降水事件的影响。我们将这场风暴的破纪录小时强度与历史记录进行了对比,并使用非平稳随机模型对其在近期到中期的风险进行了预测。这些模型的条件是三个气候模型的平均温度(T)和冷却度日(CDD)预测作为协变量,每个模型都有 SSP126 和 SSP370 情景。即使在“艾达”飓风发生之前,这种风暴发生的可能性也在缓慢增加,但非平稳模型预测的这种规模的风暴随着时间的推移再次发生的综合重现风险,比平稳模型给出的风险高 4 到 52 倍。使用 CDD 作为协变量会导致风险增加两倍以上,而使用 T 则不会。同时使用这两个协变量可以提供更广泛的不确定性范围,这凸显了为非平稳风险分析选择适当的区域协变量的重要性和细微差别。