Abstract

Abstract Mountains and plateaus in Southwest China contain many subalpine and alpine wetlands, with significant hydroecological functions. But ungauged or poorly gauged conditions limit the study and understanding of hydrological regimes of these wetland types. This study selects an ungauged subalpine wetland — Napahai in Northwest Yunnan, China — as a case for developing a practical approach to revealing its storage-area relationship of open water. A Trimble R8 GNSS (Global Navigation Satellites Systems) RTK (Real-time Kinematic system) and sonar fathometer were used to survey fine-resolution elevation data and generate a digital elevation model of the Napahai Wetland. Forty-four Landsat images from 1987 to 2011 were collected, and the Normalized Difference Water Index was used to classify open water features in the area. The area of open water in Napahai was calculated for each phase. With these data and a developed conceptual model, the storage of open water for each phase was estimated using ArcGIS tools. Both storage and area of open water showed significant intra-annual and inter-annual variations. In the rainy season, the monthly change of average storage of open water in Napahai showed about 1–2 months lag behind mean monthly rainfall. The storage-area relationship of open water was well fit by a power function equation (R 2≈0.91, n=44). This study indicates that if detailed elevations are available for similarly ungauged subalpine wetlands in Southwest China, researchers can use this practical approach to estimate multi-temporal areas and storages and reveal the storage-area relationship of open water in the wetlands. The study provided valuable information of this case wetland for optimizing its hydro-ecological managements and a new method to wetland researchers and managers for the hydrological study of similarly ungauged wetland complex.

Highlights

  • Wetlands are characterized by temporal fluctuations of water levels, and hydrology controls or affects chemical and biological processes (Deng 2007; Hollis and Thompson 1998; Krasnostein and Oldham 2004)

  • For the hydrologic year November 2001 to December 2002, Figure 4 shows that the area of open waters in Napahai had an obvious monthly fluctuation and significant variation between rainy and dry seasons

  • We found that wetlands like Napahai or the Prairie Pothole Region (PPR) depressions had strong statistical relationships between open-water V and A

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Summary

Introduction

Wetlands are characterized by temporal fluctuations of water levels, and hydrology controls or affects chemical and biological processes (Deng 2007; Hollis and Thompson 1998; Krasnostein and Oldham 2004). As hydrological response units in a catchment, wetlands have an important regulation capacity of hydrology (Mitsch and Gosselink 2007; Huang et al 2011b). Describing wetland hydrology is very important for understanding how wetland systems function and change

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