Comments on "temperature-extreme precipitation scaling: A two-way causality?"

被引:14
作者
Bao, Jiawei [1 ,2 ]
Sherwood, Steven C. [1 ,3 ]
Alexander, Lisa V. [1 ,3 ]
Evans, Jason P. [1 ,3 ]
机构
[1] Univ New South Wales, Climate Change Res Ctr, Level 4,Mathews Bldg, Sydney, NSW 2052, Australia
[2] Univ New South Wales, ARC Ctr Excellence Climate Syst Sci, Sydney, NSW, Australia
[3] Univ New South Wales, ARC Ctr Excellence Climate Extremes, Sydney, NSW, Australia
基金
澳大利亚研究理事会;
关键词
climate change; dew point temperature; extreme precipitation; extreme precipitation scaling;
D O I
10.1002/joc.5665
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Recently, Barbero et al. (2018) examined temperature-extreme precipitation scaling and argue that the local cooling effect leading to negative apparent scaling in Darwin found by Bao et al. (2017a) was simply a statistical artefact. Barbero et al. (2018) also propose that dew point temperature drives extreme precipitation, and should be used as a scaling variable. Here we address some of their criticisms and further clarify some conclusions. We maintain that scaling analyses via binning methods cannot be reliably applied to climate changes due to fundamental problems of misinterpreted causality, and that using dew point temperature does not solve these problems.
引用
收藏
页码:4661 / 4663
页数:3
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