Ice bottom evolution derived from thermistor string-based ice mass balance buoy observations-Reference-Cited by-同舟云学术

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Ice bottom evolution derived from thermistor string-based ice mass balance buoy observations

Published:2023-08-10 Issue:1 Volume:16 Page:3085-3104
ISSN:1753-8947
Container-title:International Journal of Digital Earth
language:en
Short-container-title:International Journal of Digital Earth

Author:

Liao Zeliang¹,Cheng Yubing²,Jiang Ying¹^ORCID,Li Mengmeng³,Cheng Bin⁴,Sandven Stein⁵

Affiliation:

1. School of Computer Science and Engineering, Sun Yat-Sen University, Guangzhou, People’s Republic of China

2. Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, People’s Republic of China

3. Henan Academy of Big Data, Zhengzhou University, Zhengzhou, People’s Republic of China

4. Meteorological Department, Finnish Meteorological Institute, Helsinki, Finland

5. Acoustic and Oceanography Department, Nansen Environmental and Remote Sensing Center, Bergen, Norway

Funder

the Key-Area Research and Development Program of Guangdong Province, China

the Natural Science Foundation of Guangdong Province, China

the European Union’s Horizon 2020 research and innovation program

Polar Regions in the Earth System project

Publisher

Informa UK Limited

Subject

General Earth and Planetary Sciences,Computer Science Applications,Software

Link

https://www.tandfonline.com/doi/pdf/10.1080/17538947.2023.2242326

Reference43 articles.

1. Canny, J. F. 1983. Finding Edges and Lines in Images. Cambridge: Massachusetts Institute of Technology.

2. The equivalence of best plane fit gradient with Robert's, Prewitt's and Sobel's gradient for edge detection and a 4-neighbour gradient with useful properties

3. Air/snow, snow/ice and ice/water interfaces detection from high-resolution vertical temperature profiles measured by ice mass-balance buoys on an Arctic lake

4. Evolution of snow and ice temperature, thickness and energy balance in Lake Orajärvi, northern Finland

5. Polar Amplification in Idealized Climates: The Role of Ice, Moisture, and Seasons

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