Biometeorological feedbacks on peatlands: Raising the water table to reduce meteorologically-related stress on cattle

IF 5.6 1区 农林科学 Q1 AGRONOMY Agricultural and Forest Meteorology Pub Date : 2024-11-08 DOI:10.1016/j.agrformet.2024.110279
Wanda Gherca , Inke Forbrich , Adrien Jacotot , Sara H. Knox , Paul G. Leahy , Ross Morrison , Torsten Sachs , Elke Eichelmann
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Abstract

Peatland restoration is an important mitigation action in the fight against climate change. Researchers encourage farmers to rewet deep-drained lands on organic soil to a shallow water table depth (WTD) to reduce carbon emissions. Raising WTD under grasslands will likely affect local air temperature (TA) and increase relative humidity (RH), with uncertain consequences during heat waves on cattle welfare. We used WTD, TA and RH data (both measured between 1.25 and 2 m above ground) from 22 peatland sites globally to evaluate peatlands’ overall Temperature Humidity Index (THI), an indicator correlated to cattle welfare used in dairy farms (THI>68 increases heart rate, breathing rate and reduces milk yield). We compared them with THI at state weather stations located on neighbouring lands with short grass on non-organic soil, and assessed the impact of WTD.
At most sites, peatlands with shallow WTD had lower TA, higher RH, and an overall lower THI than surrounding lands, compared to those with deep WTD. In most cases, THI decreased with increasing WTD, especially at night in the temperate region, except for coastal peatlands. Shallow and submerged sites had 20 % less hours with stressful meteorologic conditions (high THI) than surrounding areas. In contrast, the number of hours with high THI did not change significantly on peatlands with WTD under 20 cm below ground level compared to control sites. Our results confirm the influence of WTD on local temperature and THI, and suggest that raising WTD on drained peatlands will slightly improve cattle welfare with reduced THI during heat waves, but also acknowledge that local geographic characteristics add complexity to this relationship. Our research indicates that raising WTD to ground level in sections of grasslands could provide “heat wave shelters” and increase cattle resilience to climate change while contributing to the global reduction of carbon emissions.
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泥炭地的生物气象反馈:提高地下水位,减轻气象对牛的压力
泥炭地恢复是应对气候变化的一项重要减缓行动。研究人员鼓励农民将有机土壤上的深层排水土地复湿至浅地下水位深度(WTD),以减少碳排放。提高草地地下水位深度可能会影响当地气温(TA)并增加相对湿度(RH),在热浪期间会对牛的福利产生不确定的影响。我们利用全球 22 个泥炭地站点的 WTD、TA 和相对湿度数据(均在离地面 1.25 至 2 米处测量)来评估泥炭地的总体温度湿度指数(THI),这是一个与奶牛场使用的牛只福利相关的指标(THI>68 会增加心率、呼吸频率并降低产奶量)。在大多数地点,与WTD较深的泥炭地相比,WTD较浅的泥炭地的TA较低,相对湿度较高,总体THI也低于周边土地。在大多数情况下,THI 随 WTD 的增加而降低,尤其是在温带地区的夜间,沿海泥炭地除外。与周围地区相比,浅水和淹没地块的紧张气象条件(高 THI)小时数减少了 20%。相反,与对照地点相比,WTD 低于地面以下 20 厘米的泥炭地的高 THI 小时数没有显著变化。我们的研究结果证实了WTD对当地温度和THI的影响,并表明提高排水泥炭地的WTD会略微改善牛的福利,降低热浪期间的THI,但也承认当地的地理特征增加了这种关系的复杂性。我们的研究表明,将部分草地的WTD提高到地面水平可以提供 "热浪庇护所",提高牛群对气候变化的适应能力,同时为全球减少碳排放做出贡献。
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来源期刊
CiteScore
10.30
自引率
9.70%
发文量
415
审稿时长
69 days
期刊介绍: Agricultural and Forest Meteorology is an international journal for the publication of original articles and reviews on the inter-relationship between meteorology, agriculture, forestry, and natural ecosystems. Emphasis is on basic and applied scientific research relevant to practical problems in the field of plant and soil sciences, ecology and biogeochemistry as affected by weather as well as climate variability and change. Theoretical models should be tested against experimental data. Articles must appeal to an international audience. Special issues devoted to single topics are also published. Typical topics include canopy micrometeorology (e.g. canopy radiation transfer, turbulence near the ground, evapotranspiration, energy balance, fluxes of trace gases), micrometeorological instrumentation (e.g., sensors for trace gases, flux measurement instruments, radiation measurement techniques), aerobiology (e.g. the dispersion of pollen, spores, insects and pesticides), biometeorology (e.g. the effect of weather and climate on plant distribution, crop yield, water-use efficiency, and plant phenology), forest-fire/weather interactions, and feedbacks from vegetation to weather and the climate system.
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