scispace - formally typeset
J

Jun Wen

Researcher at Chengdu University of Information Technology

Publications -  135
Citations -  3621

Jun Wen is an academic researcher from Chengdu University of Information Technology. The author has contributed to research in topics: Water content & Precipitation. The author has an hindex of 27, co-authored 122 publications receiving 2590 citations. Previous affiliations of Jun Wen include United States Department of Agriculture & Jackson State University.

Papers
More filters
Journal ArticleDOI

The Tibetan plateau observatory of plateau scale soil moisture and soil temperature, Tibet - Obs, for quantifying uncertainties in coarse resolution satellite and model products

TL;DR: In this article, a plateau scale soil moisture and soil temperature observatory is established on the Tibetan plateau for quantifying uncertainties in coarse resolution satellite and model products of soil moisture, and an analysis is carried out to assess the reliability of several satellite products for the Naqu and the Maqu network areas.
Posted ContentDOI

The International Soil Moisture Network: Serving Earth system science for over a decade

Wouter Dorigo, +69 more
TL;DR: The main scope of this paper is to inform readers about the evolution of the ISMN over the past decade, including a description of network and data set updates and quality control procedures.
Journal ArticleDOI

Assessing relative soil moisture with remote sensing data: theory, experimental validation, and application to drought monitoring over the North China Plain

TL;DR: Based on physical consideration of land surface energy balance, a theory is proposed for assessing relative soil moisture in the rooting depth with remote sensing data as discussed by the authors, which is theoretically shown to be derivable from relative evaporation.
Journal ArticleDOI

An Improvement of Roughness Height Parameterization of the Surface Energy Balance System (SEBS) over the Tibetan Plateau

TL;DR: In this paper, the performance of SEBS has been tested and evaluated for typical land surfaces on the Tibetan Plateau on the basis of time series of observations at four sites with bare soil, sparse canopy, dense canopy, and snow surface, respectively.