Generalized Additive Models for Predicting Sea Level Rise in Coastal Florida

IF 2.4 Q2 GEOSCIENCES, MULTIDISCIPLINARY Geosciences (Switzerland) Pub Date : 2023-10-16 DOI:10.3390/geosciences13100310
Hanna N. Vaidya, Robert D. Breininger, Marisela Madrid, Steven Lazarus, Nezamoddin N. Kachouie
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Abstract

Within the last century, the global sea level has risen between 16 and 21 cm and will likely accelerate into the future. Projections from the Intergovernmental Panel on Climate Change (IPCC) show the global mean sea level (GMSL) rise may increase to up to 1 m (1000 mm) by 2100. The primary cause of the sea level rise can be attributed to climate change through the thermal expansion of seawater and the recession of glaciers from melting. Because of the complexity of the climate and environmental systems, it is very difficult to accurately predict the increase in sea level. The latest estimate of GMSL rise is about 3 mm/year, but as GMSL is a global measure, it may not represent local sea level changes. It is essential to obtain tailored estimates of sea level rise in coastline Florida, as the state is strongly impacted by the global sea level rise. The goal of this study is to model the sea level in coastal Florida using climate factors. Hence, water temperature, water salinity, sea surface height anomalies (SSHA), and El Niño southern oscillation (ENSO) 3.4 index were considered to predict coastal Florida sea level. The sea level changes across coastal Florida were modeled using both multiple regression as a broadly used parametric model and the generalized additive model (GAM), which is a nonparametric method. The local rates and variances of sea surface height anomalies (SSHA) were analyzed and compared to regional and global measurements. The identified optimal model to explain and predict sea level was a GAM with the year, global and regional (adjacent basins) SSHA, local water temperature and salinity, and ENSO as predictors. All predictors including global SSHA, regional SSHA, water temperature, water salinity, ENSO, and the year were identified to have a positive impact on the sea level and can help to explain the variations in the sea level in coastal Florida. Particularly, the global and regional SSHA and the year are important factors to predict sea level changes.
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预测佛罗里达沿海海平面上升的广义加性模型
在上个世纪,全球海平面上升了16到21厘米,未来可能会加速上升。政府间气候变化专门委员会(IPCC)的预测显示,到2100年,全球平均海平面(GMSL)上升可能会增加到1米(1000毫米)。海平面上升的主要原因可以归结为气候变化,这是由于海水的热膨胀和冰川的退缩而导致的。由于气候和环境系统的复杂性,准确预测海平面的上升是非常困难的。最新估计的GMSL上升约为3毫米/年,但由于GMSL是一个全球测量,它可能不代表局部海平面变化。由于佛罗里达州受到全球海平面上升的强烈影响,因此有必要对佛罗里达州海岸线的海平面上升进行量身定制的估计。这项研究的目的是利用气候因素来模拟佛罗里达沿海地区的海平面。因此,考虑水温、海水盐度、海面高度异常(SSHA)和El Niño南方涛动(ENSO) 3.4指数对佛罗里达沿海海平面的预测。采用多元回归模型和广义加性模型(GAM)对佛罗里达沿海海平面变化进行了建模,前者是一种常用的参数模型,而前者是一种非参数模型。分析了海面高度异常(SSHA)的局地率和方差,并与区域和全球测量结果进行了比较。确定的最优模型是以年、全球和区域(邻近盆地)SSHA、当地水温和盐度以及ENSO为预测因子的GAM模型。包括全球SSHA、区域SSHA、水温、盐度、ENSO和年份在内的所有预测因子都对海平面产生了积极影响,并有助于解释佛罗里达沿海海平面的变化。特别是全球和区域SSHA和年份是预测海平面变化的重要因子。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Geosciences (Switzerland)
Geosciences (Switzerland) Earth and Planetary Sciences-Earth and Planetary Sciences (all)
CiteScore
5.30
自引率
7.40%
发文量
395
审稿时长
11 weeks
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