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Trends in air temperature in Estonia and in water temperature of Estonian large lakes in 1961-2004, possible consequences on water quality

机译:1961 - 2004年爱沙尼亚气温和爱沙尼亚大湖水温度下的趋势,对水质的影响

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According to the Intergovernmental Panel on Climate Change, Fourth Assessment Report (AR4), global mean surface air temperatures (AT) have risen by 0.74 ± 0.18 °C when estimated by a linear trend over the last 100 years (1906-2005). The rate of warming over the last 50 years is almost double of that over the last 100 years (0.13 ± 0.03 °C vs. 0.07 ±0.02 per decade). Since 1979, warming has been strongest over western North America, northern Europe and China in winter; Europe and northern and eastern Asia in spring; Europe and North Africa in summer; and northern North America, Greenland and eastern Asia in autumn (TRENBERTH et al. 2007). In Estonia, annual mean AT increased during 1951-2000 by 1.0-1.7 °C. The biggest change was observed in March, when the monthly mean temperature increased by 3-5 °C (JAAGUS 2006).Water temperature and ice cover are most directly affected by climate forcing; the existence of consistent trends has been demonstrated in river water temperatures (HARI et al. 2006), lake water temperatures (LIVINGSTONE 2003, STRAILE et al. 2003, ARHONDITSIS et al. 2004, COATES et al. 2006, DOKULIL et al. 2006) and ice phenology (WEYHENMEYER et al. 2005). The physical response to local meteorological forcing is strongest in the uppermost levels of the water column and is most apparent in lake surface water temperatures ( SWT). Long-term water temperature data from the Central European lakes have been analyzed extensively, while only few data sets from Northen European lakes have been published so far. Lakes, in northern Europe have shown few significant trends in SWT compared to lakes elsewhere in Europe. No trends were found in lakes in Wisconsin in the northern USA. between 1981 and 2001 (MAGNUSON et al. 2006). Only 1 of the 8 long data series (1961-2000) for lakes in Finland showed a significant increase in SWT (KORHONEN 2002). In 8 Lithuanian lakes, the average trend of SWT was 0.5 °C dec~(-1) (PERNARAVICIUTE 2004). In Estonian lakes Vortsjarv and Peipsi, a SWT trend of 0.2-0.3 °C dec~(-1) in April and May 1948-2000 was reported by NOGES & JARVET (2005). HARI et al. (2006) showed an abrupt increase of air and river water temperature in winter, spring and summer in 1987/1988. A step jump up of water temperature took place in lakes in Austria, UK, Finland, and Sweden between 1981 and 1993, most commonly in 1988 (L. ARVOLA, unpubl. data).
机译:根据政府间气候变化问题小组第四次评估报告(AR4),全球平均气温(AT)0.74±0.18℃,当由线性趋势在过去100年(1906 - 2005)估计有所上涨。升温,在过去50年率几乎是两倍的,在过去百年(0.13±0.03℃对每十年0.07±0.02)。自1979年以来,气候变暖已经过最强的北美西部,北欧和中国冬季;欧洲北部和东部地区在春季;欧洲和北非夏季;和北美洲北部,格陵兰岛和东亚秋季变(Trenberth等,2007)。在爱沙尼亚,年平均在由1.0-1.7℃,在2051至00年增加。 3月份的时候的月平均气温上升3-5°C(2006年JAAGUS)。水的温度和冰覆盖最直接受气候强迫观察到最大的变化;的变化趋势基本一致的存在已经在河水的温度被证实(HARI等,2006),湖水的温度(LIVINGSTONE 2003,STRAILE等人。2003年,2004年ARHONDITSIS等,Coates等。2006年,DOKULIL等人。2006年)和冰物候(WEYHENMEYER等人,2005)。到本地气象迫使物理响应是最强在水柱的最上面的水平,并且在湖面水温(SWT)最为明显。从中欧湖泊长期水温数据已经被广泛分析,而来自欧洲北朝湖泊只有很少的数据集,迄今已出版。湖,北欧已经比欧洲其它地方的湖泊在SWT显示几个显著的趋势。无趋势是在湖泊在美国北部发现在威斯康星州。 1981年和2001年之间(MAGNUSON等,2006)。只有在芬兰湖泊8长的数据系列(1961-2000)的1显示在SWT一个显著上升(KORHONEN 2002)。在8个立陶宛语湖泊,SWT的平均趋势为0.5℃分解〜(-1)(2004 PERNARAVICIUTE)。在爱沙尼亚湖泊沃尔茨和Peipsi,0.2-0.3℃(分解)〜(-1)的四月和五月1948年至2000年一个SWT趋势报告NOGES&JARVET(2005)。悬垂等。 (2006年)显示,冬,春在198​​7/1988空气和河水温度的突然升高和夏季。的台阶跳水温于1988年(L. ARVOLA,unpubl。数据)发生在湖泊在奥地利,英国,芬兰和瑞典在1981年和1993年之间,最常见的。

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