English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

With global climate changes intensifying, the hydrological response toclimate changes has attracted more attention. It is beneficial not only forhydrology and ecology but also for water resource planning and management tounderstand the impact of climate change on runoff. In addition, there arelarge spatial variations in climate type and geographic characteristicsacross China. To gain a better understanding of the spatial variation of theresponse of runoff to changes in climatic factors and to detect the dominantclimatic factors driving changes in annual runoff, we chose the climateelasticity method proposed by Yang and Yang (2011). It is shown that, in mostcatchments of China, increasing air temperature and relative humidity havenegative impacts on runoff, while declining net radiation and wind speed havepositive impacts on runoff, which slow the overall decline in runoff. Thedominant climatic factors driving annual runoff are precipitation in mostparts of China, net radiation mainly in some catchments of southern China,air temperature and wind speed mainly in some catchments in northern China

Dominant climatic factors driving annual runoff changes at the catchment scale across China