Effects of changing precipitation regimes on high Arctic, tundra, ecosystems in a warming climate

气候变暖时降水状况变化对北极、苔原、生态系统的影响

• 批准号: 305521-2013
• 负责人: Henry, Gregory
• 金额: $ 1.46万
• 依托单位: University of British Columbia
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Northern Research Supplement
• 财政年份: 2013
• 资助国家: 加拿大
• 起止时间: 2013-01-01 至 2014-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=526170
• 关键词: Effects; changing; precipitation; regimes; Arctic

The Arctic is changing dramatically because of the warming climate, loss of sea ice, melting permafrost and increasing industrial development. Annual temperatures have increased by 1-4ºC and total precipitation has increased by up to 40% in the past 40 years. Tundra ecosystems are showing changes now that were seen in warming experiments in the past, such as increased growth and reproduction of plants, shifts in biodiversity, greater flows of CO2 in and out of the systems, and increased rates of soil processes and nutrient availability. Increases in plant height and cover, especially shrubs, have been measured which will impact wildlife and could lead to more warming. We have a good understanding of how tundra ecosystems respond to warming; however, the responses to the changing climate will depend on moisture conditions and whether there will be an increase or decrease in snow or rain. We know change in moisture conditions in other ecosystems is more important than change in temperature. The warming climate and loss of sea ice should result in more precipitation, and this may increase soil moisture. However, the warming will also deepen the melted layer above the permafrost and increase evaporation from the plants and soil. This could cause drier soils, despite increases in precipitation. If we are to understand and predict the changes in tundra systems we will need to know how they respond to changes in moisture conditions, and this is the focus of my proposed research. Studies will be conducted on high Arctic polar deserts. These extensive bare areas are predicted to become more vegetated. We will establish experiments in polar desert sites to increase snow depth (snow fences), soil moisture (watering) and temperature (open top greenhouses). We will also examine the role of late lying snow beds in the deserts, which supply moisture through the summer. Finally, we will reconstruct the changes in temperature and precipitation in the Canadian High Arctic over the past century from patterns in annual growth in dwarf shrubs species. Each of the studies will involve a PhD student and will significantly increase our ability to predict changes in high Arctic tundra ecosystems.

由于气候变暖、海冰消失、永久冻土融化和工业发展增加，北极正在发生戏剧性的变化。在过去的40年里，年气温上升了1-4摄氏度，总降水量增加了高达40%。苔原生态系统现在正在显示出过去在变暖实验中看到的变化，例如植物生长和繁殖增加，生物多样性发生变化，二氧化碳流入和流出系统的流量增加，土壤过程和养分可获得性增加。已经测量到植物高度和盖度的增加，特别是灌木，这将影响野生动物，并可能导致更多的变暖。我们很清楚冻土带生态系统对气候变暖的反应；然而，对气候变化的反应将取决于湿度条件以及雪或雨的增加或减少。我们知道，在其他生态系统中，水分状况的变化比温度的变化更重要。气候变暖和海冰的消失应该会导致更多的降水，这可能会增加土壤水分。然而，变暖也将加深永久冻土上方的融化层，并增加植物和土壤的蒸发。这可能会导致土壤更加干燥，尽管降雨量增加了。如果我们要了解和预测冻土带系统的变化，我们需要知道它们如何响应湿度条件的变化，这是我提议的研究的重点。将对北极高地沙漠进行研究。据预测，这些广袤的裸露地区将变得更加植被茂盛。我们将在极地沙漠地区建立增加积雪深度(雪栅栏)、土壤水分(浇水)和温度(开放式温室)的实验。我们还将研究沙漠中晚期雪层的作用，它们在整个夏天提供水分。最后，我们将根据矮小灌木物种的年生长模式重建过去一个世纪加拿大北极高地的温度和降水变化。每项研究都将涉及一名博士生，并将显著提高我们预测北极高原冻土带生态系统变化的能力。