C21E:
Frozen Soil, Its Change, and the Responses and Feedbacks of the Frozen Soil Change in Atmosphere, Hydrology, and Ecosystem I


Session ID#: 11035

Session Description:
Frozen soil is an important component of cryosphere. Atmosphere, frozen soil, water and ecosystem together form a dynamic system that is filled with responses and feedbacks. Distinctive features in atmosphere, hydrology and ecosystems are associated with the frozen soil. For example, at different thawing and freezing stages, soil surface sensible and latent heat fluxes assume dominant roles differently. Permafrost soil limits the interaction between soil surface and deep groundwater due to the hydraulic impedance. In high altitudes, the wetland ecosystem is associated with the permafrost soil. With warming climate, frozen soil degradation has been reported in the high latitudes and altitudes. Components of the dynamic system are expected to alter, and so do the responses and feedbacks among the components. In this session, we welcome studies that focus on the frozen soil modeling and observation, the mechanisms of frozen soil change, and the responses and feedbacks in the dynamic system.
Primary Convener:  Lan Cuo, ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
Conveners:  Yanhong Gao, Northwest Institute of Eco-Environment and Resources, CAS, Lanzhou, China, Shilong Piao, Peking University, Beijing, China and Lin Zhao, LZU Lanzhou University, Lanzhou, China
Chairs:  Lan Cuo, ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China and Yanhong Gao, Northwest Institute of Eco-Environment and Resources, CAS, Lanzhou, China
OSPA Liaison:  Lin Zhao, LZU Lanzhou University, Lanzhou, China

Cross-Listed:
  • A - Atmospheric Sciences
  • B - Biogeosciences
  • GC - Global Environmental Change
  • H - Hydrology
Index Terms:

0702 Permafrost [CRYOSPHERE]
0704 Seasonally frozen ground [CRYOSPHERE]
1621 Cryospheric change [GLOBAL CHANGE]
1807 Climate impacts [HYDROLOGY]

Abstracts Submitted to this Session:

Representing frozen soil and its effect on infiltration in Earth System Models (Invited) (70062)
Guo-Yue Niu, University of Arizona, Department of Hydrology and Atmospheric Sciences, Tucson, AZ, United States
Frozen Ground Controls on Hydrological Processes (Invited) (64237)
Larry D Hinzman, White House Office of Science and Technology Policy, Fairbanks, AK, United States, Douglas L Kane, University of Alaska Fairbanks, Fairbanks, AK, United States and Ming-Ko Woo, McMaster University, Hamilton, ON, Canada
Observational Evidence of Changes in Soil Temperatures across Eurasian Continent (Invited) (79916)
Tingjun Zhang, Lanzhou University, Lanzhou, China
Exploring the impacts of climate change and permafrost thaw on microlandscapes, plant species, and carbon cycling of West Siberian peatlands (Invited) (60641)
Theodore J Bohn, Arizona State University, Tempe, AZ, United States
Analysis of spatial distribution and temporal trend of soil moisture over the Tibetan Plateau from 1978 to 2013 (78296)
Xianhong Meng1, Shihua Lu2, Ruiqing Li3, Tangtang Zhang4 and Luan Lan1, (1)Cold and Arid Environmental and Engineering Research Institute, Lanzhou, China, (2)Chengdu University of Information Technology, chengdu, China, (3)Neimenggu Meteorological Observatory, huhehaote, China, (4)Chinese Academy of Sciences, Lanzhou, China
Effects of a Ground Source Heat Pump in Discontinuous Permafrost (82097)
Rorik Peterson1, Robbin Garber-Slaght1 and Ronald P Daanen2, (1)University of Alaska Fairbanks, Fairbanks, AK, United States, (2)DGGS, Fairbanks, AK, United States
The Feasibility Study of Using Microwave Emissivity in Detecting Freeze and Thaw States (80919)
Hamid Norouzi, New York City College of Technology, CUNY, Brooklyn, United States, Dr. Satya Prakash, Indian Institute of Science, Bangalore, India, Marzi Azarderakhsh, Fairleigh Dickinson University, Teaneck, NJ, United States and Reginald Blake, CUNY New York City College of Technology, Brooklyn, United States
Effects of the soil freeze−thaw process on the regional climate of the Tibet Plateau (69055)
Siqiong Luo Sr1, Boli Chen2, Shihua Lu3, Yu Zhang4 and Di Ma2, (1)Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Key Laboratory of Land Surface Process and Climate Change in Cold and Arid Regions, Lanzhou, China, (2)CAREERI/CAS Cold and Arid Regions Environmental and Engineering Research Institute, Lanzhou, China, (3)Cold and Arid Regions Eavironm, Lanzhou, China, (4)CAREERI, CAS, Lanzhou, Gansu, China

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