Infrared heater system for warming tropical forest understory plants and soils

被引:52
作者
Kimball, Bruce A. [1 ]
Alonso-Rodriguez, Aura M. [2 ]
Cavaleri, Molly A. [3 ]
Reed, Sasha C. [4 ]
Gonzalez, Grizelle [5 ]
Wood, Tana E. [2 ]
机构
[1] Greenleaf Grp, Phoenix, AZ 85018 USA
[2] US Forest Serv, Int Inst Trop Forestry, USDA, Luquillo, PR USA
[3] Michigan Technol Univ, Sch Forest Resources & Environm Sci, Houghton, MI 49931 USA
[4] US Geol Survey, Southwest Biol Sci Ctr, Moab, UT USA
[5] US Forest Serv, Int Inst Trop Forestry, USDA, Rio Piedras, PR USA
基金
美国国家科学基金会;
关键词
climate change; global warming; heater array; infrared warming; proportional integrative derivative control; trees; SUBTROPICAL WET FOREST; PERFORMANCE; CANOPY; ACCLIMATION; SIMULATION; RESPONSES; EXTREMES; ARRAYS; TUNDRA; YIELD;
D O I
10.1002/ece3.3780
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
The response of tropical forests to global warming is one of the largest uncertainties in predicting the future carbon balance of Earth. To determine the likely effects of elevated temperatures on tropical forest understory plants and soils, as well as other ecosystems, an infrared (IR) heater system was developed to provide in situ warming for the Tropical Responses to Altered Climate Experiment (TRACE) in the Luquillo Experimental Forest in Puerto Rico. Three replicate heated 4-m-diameter plots were warmed to maintain a 4 degrees C increase in understory vegetation compared to three unheated control plots, as sensed by IR thermometers. The equipment was larger than any used previously and was subjected to challenges different from those of many temperate ecosystem warming systems, including frequent power surges and outages, high humidity, heavy rains, hurricanes, saturated clayey soils, and steep slopes. The system was able to maintain the target 4.0 degrees C increase in hourly average vegetation temperatures to within +/- 0.1 degrees C. The vegetation was heterogeneous and on a 21 degrees slope, which decreased uniformity of the warming treatment on the plots; yet, the green leaves were fairly uniformly warmed, and there was little difference among 0-10cm depth soil temperatures at the plot centers, edges, and midway between. Soil temperatures at the 40-50cm depth increased about 3 degrees C compared to the controls after a month of warming. As expected, the soil in the heated plots dried faster than that of the control plots, but the average soil moisture remained adequate for the plants. The TRACE heating system produced an adequately uniform warming precisely controlled down to at least 50-cm soil depth, thereby creating a treatment that allows for assessing mechanistic responses of tropical plants and soil to warming, with applicability to other ecosystems. No physical obstacles to scaling the approach to taller vegetation (i.e., trees) and larger plots were observed.
引用
收藏
页码:1932 / 1944
页数:13
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