Novel determination of effective freeze-thaw cycles as drivers of ecosystem change

被引:5
作者
Boswell, Edward P. [1 ]
Thompson, Anita M. [2 ]
Balster, Nick J. [1 ]
Bajcz, Alex W. [3 ]
机构
[1] Univ Wisconsin, Dept Soil Sci, 1525 Observ Dr, Madison, WI 53706 USA
[2] Univ Wisconsin, Dept Biol Syst Engn, 460 Henry Mall, Madison, WI 53706 USA
[3] Drew Univ, Dept Biol, 36 Madison Ave, Madison, NJ 07940 USA
基金
美国食品与农业研究所;
关键词
NITROUS-OXIDE EMISSIONS; UNFROZEN WATER-CONTENT; SNOW REMOVAL; FOREST SOIL; TEMPERATURES; DYNAMICS; TRENDS; CARBON;
D O I
10.1002/jeq2.20053
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Soil freeze-thawcycles (FTCs) profoundly influence biophysical conditions and modify biogeochemical processes across many northern-hemisphere and alpine ecosystems. How FTCs will contribute to global processes in seasonally snow-covered ecosystems in the future is of particular importance as climate change progresses and winter snowpacks decline. Our understanding of these contributions is limited because there has been little consideration of inter- and intrayear variability in the characteristics of FTCs, in part due to a limited appreciation for which of these characteristics matters most with respect to a given biogeochemical process. Here, we introduce the concept of effective FTCs: those that are most likely linked to changes in key soil processes. We also propose a set of parameters to quantify and characterize effective FTCs using standard field soil temperature data. To put these proposed parameters into effective practice, we present FTCQuant, an R package of functions that quantifies FTCs based on a set of user-defined parameter criteria and, importantly, summarizes the individual characteristics of each FTC counted. To demonstrate the utility of these new concepts and tools, we applied the FTCQuant package to re-analyze data from two published studies to help explain over-winter changes to N2O emissions and wet-aggregate stability. We found that effective FTCs would be defined differently for each of these response variables and that effective FTCs provided a 76 and 33% increase in model fit for wet-aggregate stability and cumulative N2O emission, respectively, relative to conventional FTC quantification methods focusing on fluctuations around 0 degrees C. These results demonstrate the importance of identifying effective FTCs when scaling soil processes to regional or global levels. We hope our contributions will inform future deductions, hypothesis generation, and experimentation with respect to expected changes in freeze-thaw cycling globally.
引用
收藏
页码:314 / 323
页数:10
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