全新世中期北太平洋副热带反气旋的季节变化:中纬度斜压性的主导作用

IF 4 1区 地球科学 Q1 GEOGRAPHY, PHYSICAL
Shanshan Liu , Dabang Jiang
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引用次数: 0

摘要

了解北太平洋副热带反气旋(NPSA)变化背后的机制是解释全新世中期气候变化的关键。本文利用15个耦合模式比对项目第6阶段(CMIP6)模式的模拟,研究了全新世中期至工业化前时期的NPSA变化。结果显示出明显的季节差异:NPSA在春季减弱和收缩,但在夏季增强和扩大。这些变化源于轨道引起的经向和纬向热结构的变化,这些变化通过重新分配降水释放的潜热和改变北太平洋西风急流来调节NPSA。在春季,日照减少使北太平洋斜压带向南移动,如经向温度梯度变化所示,并减弱了陆地-海洋表面等效势温(θe)的差异。向南移动的斜压区将西风急流南移,导致NPSA中北部减弱,而海陆θe对比减弱增强了海洋对流降水,减弱了NPSA东翼。在夏季,NPSA的增强主要是由于日晒增加导致中纬度斜压性减弱导致北太平洋大尺度降水减少。今年夏季NPSA的增强还受到亚洲陆地对流降水增强和北太平洋对流降水减少的推动,这与轨道上陆地-海洋θe对比的放大有关。这项研究强调了改变的经向温度梯度的主要作用,它在很大程度上决定了大气斜压性,在形成NPSA方面,而不是以前强调的陆海热对比。该模拟合理地解释了北太平洋西部和东部代用物推断出的NPSA变化差异。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Seasonally dependent changes in the North Pacific subtropical anticyclone during the mid-Holocene: Dominant role of mid-latitude baroclinicity

Seasonally dependent changes in the North Pacific subtropical anticyclone during the mid-Holocene: Dominant role of mid-latitude baroclinicity
Understanding mechanisms behind North Pacific subtropical anticyclone (NPSA) changes is pivotal for interpreting mid-Holocene climate variations. This study investigates NPSA changes between mid-Holocene and preindustrial periods using simulations from 15 Coupled Model Intercomparison Project Phase 6 (CMIP6) models. The results reveal pronounced seasonal disparities: the NPSA weakens and contracts in spring but strengthens and expands in summer. These variations stem from orbitally induced changes in meridional and zonal thermal structures, which modulate the NPSA by redistributing precipitation-released latent heat and by altering the North Pacific westerly jet. In spring, reduced insolation shifts North Pacific baroclinic zones southward, as indicated by meridional temperature gradient changes, and attenuates land–sea contrasts in surface equivalent potential temperature (θe). The southward-shifted baroclinic zone displaces the westerly jet southward, accounting for NPSA weakening over its northern–central sector, while the attenuated land–sea θe contrast enhances oceanic convective precipitation, weakening the NPSA's eastern flank. In summer, the NPSA intensification primarily results from reduced large-scale precipitation over the North Pacific due to diminished mid-latitude baroclinicity caused by increased insolation. This summertime NPSA intensification is additionally fueled by enhanced convective precipitation over Asian land and diminished convective precipitation over the North Pacific, associated with orbitally amplified land–sea θe contrasts. This study highlights the primary role of altered meridional temperature gradients, which largely determine atmospheric baroclinicity, in shaping the NPSA, rather than the previously emphasized land–sea thermal contrasts. The simulation plausibly explains discrepancies in NPSA changes inferred from proxies in the western and eastern North Pacific.
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来源期刊
Global and Planetary Change
Global and Planetary Change 地学天文-地球科学综合
CiteScore
7.40
自引率
10.30%
发文量
226
审稿时长
63 days
期刊介绍: The objective of the journal Global and Planetary Change is to provide a multi-disciplinary overview of the processes taking place in the Earth System and involved in planetary change over time. The journal focuses on records of the past and current state of the earth system, and future scenarios , and their link to global environmental change. Regional or process-oriented studies are welcome if they discuss global implications. Topics include, but are not limited to, changes in the dynamics and composition of the atmosphere, oceans and cryosphere, as well as climate change, sea level variation, observations/modelling of Earth processes from deep to (near-)surface and their coupling, global ecology, biogeography and the resilience/thresholds in ecosystems. Key criteria for the consideration of manuscripts are (a) the relevance for the global scientific community and/or (b) the wider implications for global scale problems, preferably combined with (c) having a significance beyond a single discipline. A clear focus on key processes associated with planetary scale change is strongly encouraged. Manuscripts can be submitted as either research contributions or as a review article. Every effort should be made towards the presentation of research outcomes in an understandable way for a broad readership.
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