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首页> 外文期刊>Global change biology >Spring warming and carbon dioxide exchange over low Arctic tundra in central Canada
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Spring warming and carbon dioxide exchange over low Arctic tundra in central Canada

机译:加拿大中部低寒带苔原的春季变暖和二氧化碳交换

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摘要

Tundra-atmosphere exchanges of carbon dioxide (CO2) and water vapour were measured near Daring Lake, Northwest Territories in the Canadian Low Arctic for 3 years, 2004-2006. The measurement period spanned late-winter until the end of the growing period. Mean temperatures during the measurement period varied from about 2 degrees C less than historical average in 2004 and 2005 to 2 degrees C greater in 2006. Much of the added warmth in 2006 occurred at the beginning of the study, when snow melt occurred 3 weeks earlier than in the other years. Total precipitation in 2006 (163 mm) was more than double that of the driest year, 2004 (71 mm). The tundra was a net sink for CO2 carbon in all years. Mid-summer net ecosystem exchange of CO2 (NEE) achieved maximum values of -1.3 g C m(-2) day(-1) (2004) to -1.8 g C m(-2) day(-1) (2006). Accumulated NEE values over the 109-day period were -32,-51 and -61 g C m(-2) in 2004, 2005 and 2006, respectively. The larger CO2 uptake in 2006 was attributed to the early spring coupled with warmer air and soil conditions. In 2004, CO2 uptake was limited by the shorter growing season and mid-summer dryness, which likely reduced ecosystem productivity. Seasonal total evapotranspiration (ET) ranged from 130 mm (2004) to 181 mm (2006) and varied in accordance with the precipitation received and with the timing of snow melt. Maximum daily ET rates ranged from 2.3 to 2.7 mm day(-1), occurring in mid July. Ecosystem water use efficiency (WUEeco) varied slightly between years, ranging from 2.2 in the driest year to 2.5 in the year with intermediate rainfall amounts. In the wettest year, increased soil evaporation may have contributed to a lower WUEeco (2.3). We speculate that most, if not all, of the modest growing season CO2 sink measured at this site could be lost due to fall and winter respiration leading to the tundra being a net CO2 source or CO2 neutral on an annual basis. However, this hypothesis is untested as yet.
机译:2004-2006年,在加拿大低北极地区西北地区的达令湖附近,测量了苔原与大气之间的二氧化碳(CO2)和水蒸气交换。测量期跨度从冬季到生长期结束。测量期间的平均温度从2004年和2005年的历史平均水平低约2摄氏度到2006年的2摄氏度之间变化。2006年的大部分新增温暖发生在研究开始时,而融雪发生在3周之前比其他年份2006年的总降雨量(163毫米)是最干旱年份2004年(71毫米)的两倍多。苔原多年来一直是二氧化碳的净汇。仲夏净生态系统的CO2交换(NEE)达到-1.3 g C m(-2)day(-1)(2004)到-1.8 g C m(-2)day(-1)(2006)的最大值。在109天内,2004年,2005年和2006年的NEE累积值分别为-32,-51和-61 g C m(-2)。 2006年更多的CO2吸收归因于早春,加上空气和土壤条件变暖。在2004年,二氧化碳的吸收受到生长季节较短和仲夏干旱的限制,这可能会降低生态系统的生产力。季节性总蒸散量(ET)范围从130毫米(2004年)到181毫米(2006年),并根据收到的降水量和融雪的时间而变化。 7月中旬发生的每日最大ET排放量范围为2.3至2.7 mm day(-1)。生态系统的用水效率(WUEeco)在几年间略有变化,从最干旱的2.2到降雨量中等的2.5。在最湿润的一年中,土壤蒸发增加可能导致WUEeco降低(2.3)。我们推测,由于秋季和冬季的呼吸作用,在该地点测得的大部分(即使不是全部)适度的生长期CO2汇流失可能会导致苔原每年成为净CO2来源或CO2中性。但是,该假设尚未得到检验。

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