Anthropogenic influence on precipitation in Aotearoa New Zealand with differing circulation types

IF 6.1 1区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES Weather and Climate Extremes Pub Date : 2024-10-05 DOI:10.1016/j.wace.2024.100727
Anjali Thomas , Adrian McDonald , James Renwick , Suzanne Rosier , Jordis S. Tradowsky , Gregory E. Bodeker
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Abstract

This study quantifies the influences of anthropogenic forcing to date on precipitation over Aotearoa New Zealand (ANZ). Large ensembles of simulations from the weather@home regional climate model experiments are analysed under two scenarios, a natural (NAT) or counter-factual scenario which excludes human-induced changes to the climate system and an anthropogenic (ANT) or factual scenario. The impacts of anthropogenic forcing on precipitation are analysed in the context of large-scale circulation types characterized using an existing Self Organizing Map classification. The combined effect of both thermodynamics and dynamics are compared with values expected from the Clausius–Clapeyron (C–C) relation. Changes in the precipitation intensity due to greenhouse gas-forced temperature rise are lower than the expected C–C value. However extreme precipitation changes approach the C–C value for some circulation types. Specifically westerly flows enhance precipitation change across ANZ relative to the C–C rate, particularly over the West Coast. Conversely, northwesterly flows reduce the change over the North Island relative to the C–C value. Moreover, the wet day frequency generally reduces in the ANT scenario relative to NAT, reductions are largest on the West Coast of the South Island for westerly flows. Additionally, the frequency of days with extreme precipitation rises over ANZ for most circulation patterns, except in Northland and for northwesterly flows. This underscores the combined influence of dynamics and thermodynamics in shaping both precipitation intensity and frequency patterns across ANZ.
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不同环流类型对新西兰奥特亚罗瓦降水的人为影响
本研究量化了迄今为止人类活动对新西兰奥特亚罗瓦降水量的影响。研究分析了 "天气@家"(weather@home)区域气候模式实验在两种情景下的大型模拟集合,一种是自然情景(NAT)或反事实情景,即排除人为因素对气候系统造成的变化;另一种是人为情景(ANT)或事实情景。人为强迫对降水的影响是在大尺度环流类型的背景下利用现有的自组织地图分类特征进行分析的。热力学和动力学的综合影响与克劳修斯-克拉皮隆(C-C)关系的预期值进行了比较。温室气体导致的温度上升引起的降水强度变化低于预期的 C-C 值。然而,某些环流类型的极端降水变化接近 C-C 值。具体来说,相对于 C-C 值,西风流增强了整个澳新地区的降水变化,尤其是在西海岸。相反,相对于 C-C 值,西北气流会减少北岛的降水变化。此外,相对于 NAT,ANT 情景下的湿润日频率普遍降低,在南岛西海岸,西风流的降低幅度最大。此外,除北岛和西北气流外,在大多数环流模式下,澳新地区的极端降水日频率都有所上升。这突出表明,动力学和热力学共同影响着整个澳新地区的降水强度和降水频率模式。
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来源期刊
Weather and Climate Extremes
Weather and Climate Extremes Earth and Planetary Sciences-Atmospheric Science
CiteScore
11.00
自引率
7.50%
发文量
102
审稿时长
33 weeks
期刊介绍: Weather and Climate Extremes Target Audience: Academics Decision makers International development agencies Non-governmental organizations (NGOs) Civil society Focus Areas: Research in weather and climate extremes Monitoring and early warning systems Assessment of vulnerability and impacts Developing and implementing intervention policies Effective risk management and adaptation practices Engagement of local communities in adopting coping strategies Information and communication strategies tailored to local and regional needs and circumstances
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