The winter-spring shoulder season, or vernal window, is a key period for ecosystem carbon, water, and energy cycling. Sometimes referred to as mud season, in temperate forests, this transitional season opens with the melting of snowpack in seasonally snow-covered forests and closes when the canopy fills out. Sunlight pours onto the forest floor, soils thaw and warm, and there is an uptick in soil respiration. Scientists hypothesize that this window of ecological opportunity will lengthen in the future; these changes could have implications across all levels of the ecosystem, including the availability of food and water in human systems. Yet, there remains a dearth of observations that track both winter and spring indicators at the same location. Here, we present an inquiry-based, low-cost approach for elementary to high school classrooms to track environmental changes in the winter-spring shoulder season. Engagement in hypothesis generation and the use of claim, evidence, and reasoning practices are coupled with field measurement protocols, which provides teachers and students an authentic research experience that allows for a place-based understanding of local ecosystems and their connection to climate change.
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Winter Climate Change Reshapes Soil Climate and Biogeochemistry in a Novel Snowmelt Experiment
ABSTRACT Winter climate change is outpacing our conceptual understanding of how winter conditions regulate soil biogeochemical cycling and ultimately impact vital ecosystem services like soil carbon and nutrient retention. In seasonally snow‐covered ecosystems like northern temperate forests, increasingly inconsistent winters lead to less precipitation falling as snow, frequent midwinter snow melting, and the loss of a stable, insulative snowpack. These changes leave soils vulnerable to freezing, freeze/thaw cycling, and increasing dry/wet cycles from added snowmelt and rainwater. To uncover how these new winter soil climate conditions alter soil biogeochemistry, we introduce the DeFR❆ST (Determining Forest Responses to Snowmelt Treatments) experiment, a novel approach where we melt snow in situ throughout the winter and monitor changes to soil climate, gas exchange, and biogeochemical cycling. We installed DeFR❆ST in a New England temperate forest, an ecosystem that is part of the most significant global carbon sink and is also in the epicenter of winter climate change in the US. Experimental snow melting drove soil moisture fluctuations in addition to deep and persistent soil freezing. In turn, soils in melted plots exhibited blocked gas diffusion and lower soil oxygen availability. Oxygen limitation may have driven shifts in soil processes from high redox potential metabolisms like aerobic decomposition and nutrient mineralization towards low redox potential metabolisms like iron reduction and the dissolution of iron and carbon from organo‐mineral associations. As these changes snowball, altered soil properties and shifts in soil microbial community structure and function could reshape forest biogeochemical cycling, both in these forests and more broadly across seasonally snow‐covered ecosystems.
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- Award ID(s):
- 2237128
- PAR ID:
- 10671036
- Publisher / Repository:
- Wiley
- Date Published:
- Journal Name:
- Global Change Biology
- Volume:
- 31
- Issue:
- 8
- ISSN:
- 1354-1013
- Subject(s) / Keyword(s):
- Winter climate change climate change experiment snowmelt soil biogeochemistry soil carbon cycling upland soil redox heterogeneity soil organic matter
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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{"Abstract":["These data are from four separate projects undertaken between 1997 and\n 2017. The first of these are two snow manipulation (freeze) projects:\n 1) In 1997, as part of a study of the relationships between snow\n depth, soil freezing and nutrient cycling, we established eight 10 x\n 10-m plots located within four stands; two dominated (80%) by sugar\n maple (SM1 and SM2) and two dominated by yellow birch(YB1 and YB2),\n with one snow reduction (shoveling) and one reference plot in each\n stand. 2) In 2001, we established eight new 10-m x 10-m plots (4\n treatment, 4 reference) in four new sites; two high elevation, north\n facing and (East Kineo and West Kineo) two low elevation, south facing\n (Upper Valley and Lower Valley) maple-beech-birch stands. To establish\n plots, we cleared minor amounts of understory vegetation from all\n (both treatment and reference) plots (to facilitate shoveling).\n Treatments (keeping plots snow free by shoveling through the end of\n January) were applied in the winters of 1997/98, 1998/99, 2002/2003\n and 2003/2004.\n\n \n The Climate Gradient Project was established in October 2010. Here we\n evaluated relationships between snow depth, soil freezing and nutrient\n cycling along an elevation/aspect gradient that created variation in\n climate with little variation in soils or vegetation. We established 6\n 20 x 20-m plots (intensive plots) and 14 10 x 10-m plots (extensive\n plots), with eight of the plots facing north and twelve facing south.\n\n \n The Ice Storm project was designed to evaluate the damage and changes\n ice storms cause to northern hardwood forests in forest structure,\n nutrient cycling and carbon storage. Ten 20x30 meter plots were\n established in a predominately sugar maple stand, with 4 icing\n treatments and 2 control plots. The treatments are as follows: Low\n (0.25"), Mid (0.5"), Midx2 (0.5") 2 Years in a row,\n High: (0.75"), Control. The icing treatment was conducted in the\n winter of 2015-2016, with a second year of icing on the Midx2\n treatments plots in the winter of 2016-2017. The treatments are as\n follows: Low (0.25"), Mid (0.5"), Midx2 (0.5") 2 Years\n in a row, High: (0.75"), Control."]}more » « less
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