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揭示卫星测量数据中热带气旋降水强度增强的四十年趋势。

Unveiling four decades of intensifying precipitation from tropical cyclones using satellite measurements.

机构信息

Center for Hydrometeorology and Remote Sensing (CHRS), Department of Civil and Environmental Engineering, University of California, Irvine, Irvine, CA, USA.

Department of Earth System Science, University of California, Irvine, Irvine, CA, USA.

出版信息

Sci Rep. 2022 Aug 9;12(1):13569. doi: 10.1038/s41598-022-17640-y.

Abstract

Increases in precipitation rates and volumes from tropical cyclones (TCs) caused by anthropogenic warming are predicted by climate modeling studies and have been identified in several high intensity storms occurring over the last half decade. However, it has been difficult to detect historical trends in TC precipitation at time scales long enough to overcome natural climate variability because of limitations in existing precipitation observations. We introduce an experimental global high-resolution climate data record of precipitation produced using infrared satellite imagery and corrected at the monthly scale by a gauge-derived product that shows generally good performance during two hurricane case studies but estimates higher mean precipitation rates in the tropics than the evaluation datasets. General increases in mean and extreme rainfall rates during the study period of 1980-2019 are identified, culminating in a 12-18%/40-year increase in global rainfall rates. Overall, all basins have experienced intensification in precipitation rates. Increases in rainfall rates have boosted the mean precipitation volume of global TCs by 7-15%/year, with the starkest rises seen in the North Atlantic, South Indian, and South Pacific basins (maximum 59-64% over 40 years). In terms of inland rainfall totals, year-by-year trends are generally positive due to increasing TC frequency, slower decay over land, and more intense rainfall, with an alarming increase of 81-85% seen from the strongest global TCs. As the global trend in precipitation rates follows expectations from warming sea surface temperatures (11.1%/°C), we hypothesize that the observed trends could be a result of anthropogenic warming creating greater concentrations of water vapor in the atmosphere, though retrospective studies of TC dynamics over the period are needed to confirm.

摘要

气候变化模型研究预测,人为引起的变暖会导致热带气旋(TC)的降水率和降水量增加,在过去五年中发生的几次高强度风暴中已经发现了这种情况。然而,由于现有降水观测的限制,很难在足以克服自然气候变化的时间尺度上检测到 TC 降水的历史趋势。我们引入了一种实验性的全球高分辨率降水气候数据记录,该记录是使用红外卫星图像生成的,并通过基于测站的产品在每月尺度上进行了校正,该产品在两次飓风案例研究中表现良好,但估计热带地区的平均降水率高于评估数据集。在 1980-2019 年的研究期间,确定了平均和极端降雨率的普遍增加,最终导致全球降雨率增加了 12-18%/40 年。总体而言,所有流域的降水率都有所增强。降水率的增加使全球 TC 的平均降水总量增加了 7-15%/年,北大西洋、南印度洋和南太平洋流域的增幅最为显著(40 年内最大增幅为 59-64%)。就内陆降雨总量而言,由于 TC 频率增加、在陆地上衰减速度较慢以及降雨强度增加,年际趋势通常为正,最强的全球 TC 降雨总量增加了 81-85%,令人震惊。由于降水率的全球趋势符合变暖的海面温度(11.1%/°C)的预期,我们假设观察到的趋势可能是人为引起的变暖导致大气中水蒸气浓度增加的结果,尽管需要对该时期的 TC 动力学进行回顾性研究来证实这一点。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8453/9363467/f7f0ae564dbb/41598_2022_17640_Fig1_HTML.jpg

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