Weyhenmeyer G A
Department of Environmental Assessment, Swedish University of Agricultural Sciences, P.O. Box 7050, SE-750 07 Uppsala, Sweden.
Ambio. 2001 Dec;30(8):565-71. doi: 10.1579/0044-7447-30.8.565.
Winters in Sweden have become warmer in the 1990s, and as a consequence the timing of ice break-up and the growth and decline of spring phytoplankton has shifted, starting earlier. Even spring temperatures have become warmer, leading to an earlier beginning of the summer phytoplankton growth. The spring-ward shift in phytoplankton population growth has resulted in an extension of the growing season by at least one month. Although mean total phytoplankton biomass from May to October has not increased, the spring and early summer biomass of temperature-sensitive phytoplankton groups, such as cyanobacteria and chlorophytes, has increased in the 1990s. No increase was noted for other phytoplankton groups. Considering that some species of cyanobacteria that commonly occur during a summer bloom, such as Anabaena, Aphanizomenon, and Microcystis, can be toxic, the effect of warmer winters on aquatic ecosystems is potentially far-reaching.
20世纪90年代,瑞典的冬季变得更温暖,结果冰面破裂的时间以及春季浮游植物的生长和衰退时间都发生了变化,开始得更早。甚至春季气温也变得更高,导致夏季浮游植物生长更早开始。浮游植物种群生长向春季的转变使生长季节延长了至少一个月。尽管5月至10月浮游植物的平均总生物量没有增加,但对温度敏感的浮游植物群体,如蓝藻和绿藻,在20世纪90年代的春季和初夏生物量有所增加。其他浮游植物群体则未见增加。鉴于一些在夏季水华中常见的蓝藻物种,如鱼腥藻、束丝藻和微囊藻,可能有毒,暖冬对水生生态系统的影响可能是深远的。