Jiang water storage project

Inferring decelerated land subsidence and

We then retrieve the spatial–temporal variations of total groundwater storage, recoverable groundwater storage, and irreversible groundwater storage. Groundwater storage depletion rates are apparently

Jiang JIANG | Professor | PhD | Nanjing Forestry

Food and water security are crucial for sustainable development in arid regions. However, land use/cover change often leads to trade-offs between grain yield and water-related ecosystem services

Lake water storage estimation method based on similar

By penetrating the water body with a green band laser, airborne Lidar is an efficient method for mapping the water depth (Crétaux et al., 2005, Crétaux et al., 2011, Crétaux et al.,

A review of salt precipitation during CO2 injection into saline

The issue of salt precipitation during CO2 geological storage in saline aquifers has presented significant challenges to the injectivity of current CO2 geological storage projects.

Separating the Precipitation‐ and

In contrast, anthropogenic activities (agricultural irrigation, industrial water use, etc.) and accelerated glacial melting due to global warming are the dominant factors in the decline of water storage; (c) the contribution of

Terrestrial Water Storage in China:

China is the largest agricultural country with the largest population and booming socio-economy, and hence, remarkably increasing water demand. In this sense, it is practically critical to obtain knowledge about spatiotemporal

Different Types of Water Storage | Download

Download Table | Different Types of Water Storage from publication: Scale issues in the governance of water storage projects | In the face of global change, which is characterized by growing water

Detection of the spatial patterns of water storage variation over China

Here, we aimed to present long-term spatial patterns of TWS over China between 1948 to 2015 by unique Global Land Data Assimilation System Version 2 data and identify

Jiang water storage project [PDF]

6 FAQs about [Jiang water storage project]

Does water storage change over China between 1948 to 2015?

Here, we aimed to present long-term spatial patterns of TWS over China between 1948 to 2015 by unique Global Land Data Assimilation System Version 2 data and identify possible factors to water storage changes. The results revealed that the inner-annual variations in TWS of China exhibited remarkable downward trends with decreased rate of 0.1 cm/yr.

Will human intervention stabilize groundwater storage across the North China Plain?

Yang W, Long D, Scanlon B R, et al. Human intervention will stabilize groundwater storage across the North China Plain. Water Resources Res, 2022, 58: e2021WR030884 Yang Y, Yang Y, Moiwo J P, et al. Estimation of irrigation requirement for sustainable water resources reallocation in North China. Agric Water Manage, 2010, 97: 1711–1721

Where does water storage increase in China?

Specifically, Northeast China, the YR, and Southwest China, where deeper reservoirs predominate, witnessed a significant rise in total water storage, whereas the shallower reservoir-dominated Eastern China and Northwest China reported declining water storage.

Do water resources management measures affect land water storage?

Several water resources management measures have been implemented in recent decades to alleviate groundwater depletion, maintain ecological resilience, and sustain agricultural production. This study aims to investigate their impacts on land water storage, and thus obtain a picture of the spatio-temporal variation of water resources over the NCP.

Does total water storage continuously decrease in North China Plain (NCP)?

In this study, multi-satellite products and modeled variables were used to investigate the total water storage (TWS) and the dynamics of its components in the North China Plain (NCP). The main conclusions of this study are: The spatial pattern of TWSA indicates that the water storage continuously decreased in most parts of NCP.

How fast does water storage increase in Northeast China?

In Northeast China (NE), large reservoirs witnessed an expansion in both inundated area and water storage, with rates of 113 ± 20 km 2 per year (2.9 ± 0.5% per year) and 3.2 ± 0.6 km 3 per year (4.0 ± 0.8% per year) over the entire study period.

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