Evidence map›Paper›PMID 32368709›Full record

ArticleGeoHealth2020

Quantifying the Effect of Xiluodu Reservoir on the Temperature of the Surrounding Mountains.

D C Wang, J Y Liu, Y Huang, X W Duan, X Wang, X Zhang, Z C Sun, J H Chen, W Zhang

Open access · goldAbstract read
In one paragraph

Article in GeoHealth, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 2 papers.

0numbers the graph read from it
0cells of the map it votes in
2citing papers in PubMed
0.3field-weighted citation impact, top 46% of its field
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

2 citing papers in PubMed, 6 citations in OpenAlex.

  1. Article
  2. Article
4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

9 authors at 2 institutions in 1 country.

D C WangSchool of Geology and Geomatics Tianjin Chengjian University Tianjin China.ORCID https://orcid.org/0000-0001-7422-4291
J Y LiuSchool of Geology and Geomatics Tianjin Chengjian University Tianjin China.
Y HuangInstitute of International Rivers and Eco-Security Yunnan University Kunming China.
X W DuanInstitute of International Rivers and Eco-Security Yunnan University Kunming China.ORCID https://orcid.org/0000-0003-0183-910X
X WangSchool of Geology and Geomatics Tianjin Chengjian University Tianjin China.
X ZhangSchool of Geology and Geomatics Tianjin Chengjian University Tianjin China.
Z C SunSchool of Geology and Geomatics Tianjin Chengjian University Tianjin China.
J H ChenSchool of Geology and Geomatics Tianjin Chengjian University Tianjin China.
W ZhangSchool of Geology and Geomatics Tianjin Chengjian University Tianjin China.
Tianjin Chengjian University · CNYunnan University · CN

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

To quantitatively determine the effect of Xiluodu Reservoir on the temperature of the surrounding mountains, the temperature differences between various locations and the reservoir were calculated based on Landsat 8 thermal infrared sensor (TIRS) data. Elevation, slope, aspect, normalized difference vegetation index (NDVI), and visual field were selected as the impact factors, and the most significant grid size used to explore the effect of reservoir on the surrounding mountains was determined by spatial analysis and partial correlation analysis. The effect of the Xiluodu Reservoir on the surrounding mountains' temperature was then quantitatively studied while accounting for the effect of water surface width on temperature. The results are summarized as follows. The most significant grid size for determining the influence of Xiluodu Reservoir on the surrounding mountains' temperature is 90 m. The effect range threshold of the entire reservoir on the temperature of the surrounding mountains is approximately 600 m, and the partial correlation coefficient in each buffer area decreases gradually with increasing distance from the reservoir. The effect threshold of the reservoir on the temperature of the surrounding mountains is approximately 1,500 m in the head area with a water surface width approximately 1,000 m, but it is negligible in the tributary area where the width is approximately 60 m.

Indexed as

effect thresholdfactor analysispartial correlation analysistemperature differencesXiluodu Reservoir

Identifiers

PMID32368709
PMCPMC7195805
OpenAlexW3011220288

What OpenQuestion holds

Textmetadata
LicenceCC BY
Read underepoch 390

Registered trials

None linked

Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.