The climate of a region, an encompassing manifestation of long-term weather patterns, holds significant importance (Abbass et al.,
2022). Traditionally evaluated across a span of three decades, these patterns underpin a region’s climate identity. Over the span of the last 65 ten thousand years, the Earth has undergone natural shifts between ice ages and warm eras, altering its climate rhythm. These shifts, governed by the planet’s energy equilibrium, encompass intricate variables such as solar fluctuations, orbital dynamics, oceanic currents, albedo reflections, and atmospheric composition (UNEP,
2019). However, what distinguishes our exploration lies in the contemporary context of anthropogenic transformation (Olabi and Abdelkareem,
2022). With the planet immersed in the industrial revolution and presently traversing the era of Industry 4.0, an unprecedented surge in human activity has catalyzed global warming over the past century (Kemp et al.,
2022). As temperature rises and glaciers melt at an accelerated pace, the terrain transforms. Notably, this dynamic interplay between human interventions and planetary responses has the potential to reshape essential components of terrestrial ecosystems (Xiong et al.,
2021). While public discourse often centers on economic and ecological risks, it is the subtleties within the ancient ice cores that truly capture our attention. Unveiling echoes of climatic epochs dating back 80 ten thousand years, these cores bear witness to the intricate relationship between rising carbon dioxide levels and soaring temperatures (Mora et al.,
2022). Amidst this intricate tapestry of Earth’s climate narrative, the Himalayan region emerges as a protagonist. Revered as the “third pole” and the “water tower of Asia”, this remarkable mountain expanse boasts an ice and snow cover rivaled only by polar realms (Xu et al.,
2009). What sets our study apart is the fusion of historical significance with the immediacy of change (Shukla et al.,
2022). In the heart of the Greater Himalaya, climate change’s impact reverberates palpably (Beniston,
2003). As glaciers rapidly recede, the specter of future water scarcity looms large downstream, prompting collective concern (Yao et al.,
2004). While the 20th century witnessed marked climate fluctuations, the 21st century's onset has seen a four-fold acceleration in warming trends (Yan and Liu,
2014). Yet, our pursuit extends beyond temperature statistics. The symphony of climate alteration orchestrates cascading effects, touching realms of water availability, biodiversity, ecosystem dynamics, and global feedback. As snows melt and monsoons shift, as carbon seeps from thawing soils, intricate ecosystems and societal fabrics are rewoven (Xu et al.,
2009). In the heart of this evolving narrative, the Himalayan communities grapple with profound transformation (Jones et al.,
2022). Agriculture falters in the absence of glacial rivers, compelling shifts to non-primary livelihoods (Xu et al.,
2009). Thus, the enigma of melting ice transcends ecological implications, permeating realms of agriculture, hydropower, and the very essence of human existence—from livelihoods to spiritual connections. However, as glaciers melt, mysteries unfold. The ramifications of this glacier runoff dance remain largely obscured, a puzzle whose pieces we strive to fit together. Presently, existing studies rely on conjecture rather than concrete evidence, leaving the intricate interplay of melting glaciers, mountain hydrology, and human societies a realm yet to be fully illuminated (Carey et al.,
2017). In this synthesis of ancient rhythms and contemporary melodies, our exploration embarks on the quest to unravel the profound novel realities that climate change has woven into the fabric of the Himalayas (Parmesan et al.,
2022).