US EditionPublished • loading... • Updated
Soil moisture and atmospheric dryness govern regional controls of land–atmosphere water and heat fluxes on the Tibetan Plateau
Summary by researchsquare.com
This story is only covered by news sources that have yet to be evaluated by the independent media monitoring agencies we use to assess the quality and reliability of news outlets on our platform. Learn more here.1 Articles
1 Articles
Soil moisture and atmospheric dryness govern regional controls of land–atmosphere water and heat fluxes on the Tibetan Plateau
Water and heat flux exchanges over the Tibetan Plateau strongly affect Asian and global climate, yet sparse observations leave their controlling mechanisms poorly understood. Using eddy-covariance data from 19 sites, we identify the controls on latent (LE) and sensible (H) heat fluxes and eval...
Coverage Details
Total News Sources1
Leaning Left0Leaning Right0Center0Last UpdatedBias DistributionNo sources with tracked biases.
Bias Distribution
- There is no tracked Bias information for the sources covering this story.
Factuality
To view factuality data please Upgrade to Premium
