Evaluation of Long-Term Air and Soil Temperature Changes on the Far North-East of Russia

Long-term temperature conditions of 3,2 m thick soil layer are studied based on the data of Transbaikalian weather stations. Among all the thermal factors, the most informative one, the smallest monthly mean temperature in the annual cycle at the standard measurement depth, is used. Its vertical profiles reflect the depth variations of the temperature and its spatial diversity. They constitute the base for a newly developed graphical classification scheme for wintery thermal conditions of soils. It includes five types of the thermal conditions

show abstract

Modern Changes in the Thermal Regime of Mountain Rivers in the Permafrost Zone (A Case Study for the Upper Kolyma)

Ushakov

Ukhov

2020

Russ. Meteorol. Hydrol.

View full text Add to dashboard Cite

scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.

Contact Info

customersupport@researchsolutions.com

10624 S. Eastern Ave., Ste. A-614

Henderson, NV 89052, USA

This site is protected by reCAPTCHA and the Google Privacy Policy and Terms of Service apply.

Blog Terms and Conditions API Terms Privacy Policy Contact Cookie Preferences Do Not Sell or Share My Personal Information

Made with 💙 for researchers

Part of the Research Solutions Family.

Evaluation of Long-Term Air and Soil Temperature Changes on the Far North-East of Russia

Cited by 4 publications

References 0 publications

Soil Temperature of Steppe Landscapes in the South of Eastern Siberia and Its Response to Climate Change

Soil Temperature of Steppe Landscapes in the South of Eastern Siberia and Its Response to Climate Change

Approaches to mapping the soils’ thermal regime under the conditions of Transbaikalia’s contrasting relief

Modern Changes in the Thermal Regime of Mountain Rivers in the Permafrost Zone (A Case Study for the Upper Kolyma)

Contact Info

Product

Resources

About