Aeolian Dust Dynamics in Asia and their Teleconnection with Abrupt Climate Events in the Northern Hemisphere during the last 130.000 years: palaeoclimatic processes, feedbacks and impacts on Earths climate system

理解末次冰期的温度突变和千年尺度的气候振荡，即Dansgaard-Oeschger （DO）事件，是第四纪古气候学的一个突出问题。对格陵兰冰芯的高分辨率研究指出，在格陵兰岛突然变暖（DO事件）发生之前，格陵兰岛的沙尘沉降略显减少，这反映了亚洲沙漠的隐性干旱，从而减少了从亚洲沙尘源向北半球暴发的大陆沙尘。确定导致亚洲干旱波动的天气性大气过程，并解释为什么这些动力学与格陵兰冰芯记录的DO事件一致，或者更重要的是，稍微早于DO事件，仍然是一个紧迫的问题。大气中的矿物粉尘在气候变化中起着重要作用，既是气候变化的产物，也是气候变化的原因。矿物粉尘一旦沉积，就会提供过去气候和大气环流的记录。中亚和东亚高山丘陵和前陆的厚黄土序列是唯一的陆相气候档案和亚洲冰期间冰期和次千年沙尘运移动力学变化的原始记录。黄土记录提供了一个独特的洞察气候驱动的大陆沙尘负荷在北半球的主要来源。该项目旨在测试格陵兰岛记录的气候突变与亚洲沙尘源地区相关气候动态之间的假设联系。此外，该项目的目的是调查亚洲中部和高山在多大程度上是欧亚大陆内陆敏感的冰川-沙漠-沙尘响应系统中的一个关键因素，以及它们在多大程度上可以被认为是亚轨道全球气候变化的起跑者和北半球气候突变振荡的发起者。本文将对塔吉克斯坦西部、塔克拉玛干沙漠边缘和中国黄土高原的高分辨率黄土记录进行分析，以获得与亚洲中部和高海拔山脉周边大气环流系统相关的区域大尺度风成输运动力学和变率的理解。将已建立的可靠的亚洲沙尘代理记录与北半球其他高分辨率气候记录联系起来并相互关联是该项目的主要目标，并将增加对陆地-大气-海洋相互作用和过程的了解。后者对于理解过去气候变化中的周期性相互作用和复杂反馈是必不可少的，因此对于确定北半球大气环流的天气古气候模式至关重要，这是理解过去13万年地球气候系统突变气候动力学的驱动因素和触发因素的关键

Understanding abrupt temperature shifts and millennial-scale climate oscillations, known as Dansgaard-Oeschger (DO) events, during the last glaciation, is an outstanding question in Quaternary paleoclimatology. High-resolution studies on Greenland ice cores pointed out that the onsets of abrupt Greenland warmings (DO events) were slightly preceded by decreasing Greenland dust deposition, reflecting a recessive aridity in the Asian deserts and thus reduced continental dust outbreaks into the Northern Hemisphere from the Asian dust sources. It remains a pressing problem to identify the synoptic atmospheric processes that account for the aridity swings in Asia and to decipher why those dynamics are coherent with, or moreover, slightly preceding DO events recorded in Greenland ice cores.Mineral dust in the atmosphere plays an important role in modifying climate, being both a product and a cause of climate change. Once deposited, accumulations of mineral dust provide a record of past climate and atmospheric circulation. The thick loess sequences found along the foothills and forelands of the central and east Asian high mountains are the only terrestrial climate archive and prime recorder of glacial-interglacial and sub-millennial changes in Asian dust transport dynamics. Loess records provide a unique insight into the climate driven continental dust load in the Northern Hemisphere at its major source. The project aims to test hypothesized links between abrupt climate variability recorded in Greenland and associated climate dynamics at Asian dust source areas. Furthermore, the project is designed to investigate to what extent the central and high Asian mountains are a crucial element within the sensitive glacier-desert-dust response system in interior Eurasia and to what extent they may be considered a pacemaker of suborbital global climate changes and an initiator of abrupt climate oscillations in the Northern Hemisphere.High resolution loess records in western Tajikistan, at the fringe of the Taklamakan Desert, and the Chinese Loess Plateau will be analyzed in order to derive an understanding of regional, large-scale aeolian transport dynamics and variability related to atmospheric circulation systems operating in the immediate circumference of the central and high Asian mountain ranges. Linking and correlating the established robust Asian dust proxy records with other high resolution climate records in the Northern Hemisphere constitutes a major aim of the project and will add to the knowledge about the land-atmosphere-ocean interactions and processes. The latter is indispensable for the understanding of recurrent interactions and complex feedbacks in past climate changes and thus fundamentally important to identify synoptic paleoclimatic patterns of atmospheric circulation in the Northern Hemisphere, which holds the key to understand drivers and triggers of abrupt climate dynamics in Earths climate system during the last 130.000 years