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hg30717580木蟲 (職業(yè)作家)
總經(jīng)理
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[求助]
求助翻譯幾個(gè)圖表上的標(biāo)題
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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) |

木蟲 (正式寫手)
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(圖1)這種時(shí)間溫度模式表明,第一個(gè)明顯的季節(jié)性溫度下降后首次形成冰腳,隨后溫度上升到零上(正值),冰腳破裂,露出潮間帶。之后,冬天到了,持續(xù)七周的時(shí)間里氣溫幾乎都是在零度以下(圖1),到二月中旬,潮間帶被覆蓋了厚厚的、堅(jiān)固的一層冰(Fig. 2A),海表面同樣覆蓋著冰。在冰腳以下,溫度的波動(dòng)比較小。在2月6日到3月10日,潮間帶溫度只在−2.4°和−1.1°之間變化,但在海岸上溫度在−18.9℃和8.3℃之間(圖1)。在這期間以后,氣溫頻繁地再一次上升到零上,這給潮間帶的溫度造成了較大的變動(dòng)(圖1)。這一時(shí)期的累積同時(shí)破壞了冰腳(Fig. 2B)。該階段統(tǒng)計(jì)數(shù)據(jù)見表1。 表1 2007年1月4日和4月4日,新斯科舍省,Spray Shore海潮間帶和干燥海岸的溫度(℃)統(tǒng)計(jì)(溫度每小時(shí)記錄一次) |

木蟲 (職業(yè)作家)
總經(jīng)理
送鮮花一朵 |
謝謝您哈!還有一小段忘了復(fù)制了:能再麻煩下您嗎?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 |

木蟲 (正式寫手)
| 在記錄部署后的最初一段時(shí)間,零上溫度主要發(fā)生Spray Shore海的潮間帶和空中的位置,隨著冬季的到來,零上溫度與零下溫度交替越來越頻繁(圖1)。由于漲潮和退潮時(shí)波動(dòng)的抑制效果,在潮間帶,溫度波動(dòng)比在干燥的海岸的溫度波動(dòng)要低。第一次較大的降溫事件發(fā)生在1月18日,空氣溫度下降到 - 16.1℃,緊接著潮間帶出現(xiàn)個(gè)歷時(shí)比較短的、但是屬于標(biāo)志性的溫度變動(dòng)下降(圖1)。隨后1月19日,氣溫上升至7.7°C,使潮間帶的溫度恢復(fù)了較高的變異。 |

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