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hg30717580

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(Fig. 1). Such a temporal pattern in temperature suggests that the ice foot formed by first time after the first pronounced seasonal drop in temperature and that, after the subsequent rise to positive values, the ice foot brokedown, exposing the intertidal zone again.After that time, full winter conditions settled and air temperature remained almost always negative for seven weeks (Fig. 1 ). By mid -February, the intertidal zone was covered by a thick, stable layer of ice( Fig. 2A); the sea surfa ce was covered by ice as well.Under the ice foot, temperature f luctuations were small. Bet ween 6 Fe bruary and 10 March, temperature ranged only between − 2.4 °C and − 1.1 °C at the intertida l zone, but between − 18.9 °C and 8.3 °C at the dry coast ( Fig. 1). After this period, air temperature frequently switched to positive values again, which was again followed by temperature regaining a higher variability at the intertidal zone ( Fig. 1). This period coincided with the progressive break- up of the ice foot
( Fig. 2B). Descript ive stat istics for the full study periodare given in Table 1


Table 1
Descriptive statistics for temperature (°C) at the intertidal zone and at the dry coast at Sea Spray Shore, Nova Scotia, between 4 January and 4 April 2007 (temperature was recorded every hour)

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chem小笨

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hg30717580(金币+20): ★★★★★最佳答案, 非常感谢您!!! 2012-03-13 18:53:04
在记录部署后的最初一段时间,零上温度主要发生Spray Shore海的潮间带和空中的位置,随着冬季的到来,零上温度与零下温度交替越来越频繁(图1)。由于涨潮和退潮时波动的抑制效果,在潮间带,温度波动比在干燥的海岸的温度波动要低。第一次较大的降温事件发生在1月18日,空气温度下降到 - 16.1℃,紧接着潮间带出现个历时比较短的、但是属于标志性的温度变动下降(图1)。随后1月19日,气温上升至7.7°C,使潮间带的温度恢复了较高的变异。
发上等愿,结中等缘,享下等福;择高处立,就平处坐,向宽处行。
4楼2012-03-13 14:47:18
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chem小笨

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爱与雨下(金币+1): 2012-03-13 14:14:59
爱与雨下(金币+2): 2012-03-13 14:15:06
hg30717580(金币+20, 翻译EPI+1): ★★★★★最佳答案, 还有一段希望能帮我一下啊。。。 2012-03-13 14:24:50
(图1)这种时间温度模式表明,第一个明显的季节性温度下降后首次形成冰脚,随后温度上升到零上(正值),冰脚破裂,露出潮间带。之后,冬天到了,持续七周的时间里气温几乎都是在零度以下(图1),到二月中旬,潮间带被覆盖了厚厚的、坚固的一层冰(Fig. 2A),海表面同样覆盖着冰。在冰脚以下,温度的波动比较小。在2月6日到3月10日,潮间带温度只在−2.4°和−1.1°之间变化,但在海岸上温度在−18.9℃和8.3℃之间(图1)。在这期间以后,气温频繁地再一次上升到零上,这给潮间带的温度造成了较大的变动(图1)。这一时期的累积同时破坏了冰脚(Fig. 2B)。该阶段统计数据见表1。

表1
2007年1月4日和4月4日,新斯科舍省,Spray Shore海潮间带和干燥海岸的温度(℃)统计(温度每小时记录一次)

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2楼2012-03-13 13:27:24
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: Originally posted by chem小笨 at 2012-03-13 13:27:24:
(图1)这种时间温度模式表明,第一个明显的季节性温度下降后首次形成冰脚,随后温度上升到零上(正值),冰脚破裂,露出潮间带。之后,冬天到了,持续七周的时间里气温几乎都是在零度以下(图1),到二月中旬,潮 ...

谢谢您哈!还有一小段忘了复制了:能再麻烦下您吗?Initially after logger deployment, mostly positive tem-peratures occurred in intertidal and aerial locations at Sea Spray Shore, increasingly alternating with negative values as the winter progressed ( Fig. 1) . Temperature fluctuations were generally lower at the intertidal zone than at the dry coast (tree branches) because of the dampening effects of high tides and wave action at low tides. The first major cooling event occurred on 18 January, when air tem-perature dropped to − 16.1 °C, which was closely followed by a brief, but marked, decrease in temperature variability at the intertidal zone (Fig. 1). The following rise in air temperature to 7.7 °C on 19 January resulted in intertidal temperature regaining a higher variability
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3楼2012-03-13 14:09:31
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