Abstract
Abstract. Glaciers in the Pamir Mountains are generally acknowledged to be in a stable state and show the least glacial retreat in high-mountain Asia; however, they are also some of the most dynamic glaciers in the region and their behaviour has been spatially variable in recent decades. Few data exist for these glaciers, in particular relating to how they are responding to recent climatic changes. Here, we utilize Landsat 7 (ETM+), Landsat 8 (OLI), ASTER, and Google Earth optical images acquired between 1999 and 2016 to characterize the dynamics of the glaciers in the Kingata Mountains, located in the eastern Pamir Mountains. We quantify the velocity, areal, and frontal changes of these glaciers, which provide us with valuable data on their recent dynamic evolution and an indication of how they may evolve in future years. We highlight 28 glaciers among which 17 have changed markedly over the study period. We identify four advancing glaciers and 13 surge-type glaciers. The dynamic evolution of the glacier surges shows some similarity with those of the nearby Karakoram, suggesting that both hydrological and thermal controls are important for surge initiation and recession. Topography seems to be a dominant control on non-surge glacier behaviour in the Kingata Mountains, with the north side of the divide characterized by steep, avalanche-fed basins and glacier tongues now approaching recession in contrast to those on the south side of the divide that capture the majority of precipitation and have much broader plateau-like accumulation zones. This study is the first synthesis of glacial motion across this region and provides a baseline with which to compare future changes.
Highlights
Changes in mountain glaciers represent a key indicator of climate variability, as well as contributing to sea-level-rise and at times being the source of flood hazards (Oerlemans, 1994; Meier et al, 2007; Burgess et al, 2013; Gardner et al, 2013)
In the far west, the eastern Pamir Mountains are characterized by relatively stable glaciers and, there remains debate within the literature regarding the details (Khromova et al, 2006; Bolch et al, 2012; Kääb et al, 2012; Farinotti et al, 2015), recent research has revealed that Pamir, along with the nearby Karakoram, is the region of transition from positive to negative mass balance, with the eastern Pamir Mountains experiencing a slight positive mass balance in the early twenty-first century
We suggest that surges in the eastern Pamir Mountains, as with surges in Karakoram, have variable controlling processes depending on the thermal and hydrological conditions, and the geomorphological characteristics of different individuals
Summary
Changes in mountain glaciers represent a key indicator of climate variability, as well as contributing to sea-level-rise and at times being the source of flood hazards (Oerlemans, 1994; Meier et al, 2007; Burgess et al, 2013; Gardner et al, 2013). Since the 1990s, the glaciers in HMA have broadly been in recession, and the glacier mass balance has been negative (Yao et al, 2004; Tian et al, 2006). In the far west, the eastern Pamir Mountains are characterized by relatively stable glaciers and, there remains debate within the literature regarding the details (Khromova et al, 2006; Bolch et al, 2012; Kääb et al, 2012; Farinotti et al, 2015), recent research has revealed that Pamir, along with the nearby Karakoram, is the region of transition from positive to negative mass balance, with the eastern Pamir Mountains experiencing a slight positive mass balance in the early twenty-first century Lv et al.: Characterizing the behaviour of glaciers in the Kingata Mountains al., 2012, 2013; Gardner et al, 2013; Osmonov et al, 2013; Holzer et al, 2015; Kääb et al, 2015; Brun et al, 2017)
Sign-in/Register to view highlights & summary Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
