Abstract

The warming climate is threatening to alter inland water resources on a global scale. Within all waterbody types, lake and river systems are vital not only for natural ecosystems but, also, for human society. Snowmelt phenology is also altered by global warming, and snowmelt is the primary water supply source for many river and lake systems around the globe. Hence, (1) monitoring snowmelt conditions, (2) tracking the dynamics of snowmelt-influenced river and lake systems, and (3) quantifying the causal effect of snowmelt conditions on these waterbodies are critical to understand the cryo-hydrosphere interactions under climate change. Previous studies utilized in-situ or multispectral sensors to track either the surface areas or water levels of waterbodies, which are constrained to small-scale regions and limited by cloud cover, respectively. On the contrary, in the present study, we employed the latest Sentinel-1 synthetic aperture radar (SAR) and Sentinel-3 altimetry data to grant a high-resolution, cloud-free, and illumination-independent comprehensive inland water dynamics monitoring strategy. Moreover, in contrast to previous studies utilizing in-house algorithms, we employed freely available cloud-based services to ensure a broad applicability with high efficiency. Based on altimetry and SAR data, the water level and the water-covered extent (WCE) (surface area of lakes and the flooded area of rivers) can be successfully measured. Furthermore, by fusing the water level and surface area information, for Lake Urmia, we can estimate the hypsometry and derive the water volume change. Additionally, for the Brahmaputra River, the variations of both the water level and the flooded area can be tracked. Last, but not least, together with the wet snow cover extent (WSCE) mapped with SAR imagery, we can analyze the influence of snowmelt conditions on water resource variations. The distributed lag model (DLM) initially developed in the econometrics discipline was employed, and the lagged causal effect of snowmelt conditions on inland water resources was eventually assessed.

Highlights

  • Inland water resources play an essential role in the prosperity and stability of human society but, the sustainability and balance of various ecosystems

  • The importance of snowmelt water to downstream freshwater is widely recognized. Assessing this cryo-hydrosphere interaction is indispensable to understand the future trend of water resources we have in severer climate change scenarios

  • Since the goal of the present study is to (1) monitor the dynamics of inland waterbodies and (2) quantify the lagged influence of snowmelt on inland water dynamics, we selected the study sites based on the following criteria: (1) their spatial scales were wide enough to be detected by spaceborne synthetic aperture radar (SAR) and altimetry sensors, (2) they demonstrated a considerable magnitude of variations in both water level and surface area, and (3) their watersheds included snow-covered regions

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Summary

Introduction

Inland water resources play an essential role in the prosperity and stability of human society but, the sustainability and balance of various ecosystems. The importance of local rivers and lakes should be noted, as they are critical freshwater sources for many regions [3] and, influence the climate [4]. The importance of snowmelt water to downstream freshwater is widely recognized. Assessing this cryo-hydrosphere interaction is indispensable to understand the future trend of water resources we have in severer climate change scenarios. Monitoring snowmelt conditions and the dynamics of snowmelt-influenced river and lake systems and quantifying the causal effect of snowmelt water on these waterbodies are critical. It would allow us to understand the impact of global warming to inland water resources but, to assess the vulnerability and variability of regional freshwater supplies

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