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首页> 外文期刊>Geophysical Research Letters >REGIONAL TRENDS OF SURFACE AND TROPOSPHERIC TEMPERATURE AND EVENING-MORNING TEMPERATURE DIFFERENCE IN NORTHERN LATITUDES - 1973-93
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REGIONAL TRENDS OF SURFACE AND TROPOSPHERIC TEMPERATURE AND EVENING-MORNING TEMPERATURE DIFFERENCE IN NORTHERN LATITUDES - 1973-93

机译:北部海平面和对流层温度的区域趋势和傍晚温度差异-1973-93

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摘要

Trends for the 21-year period 1973-1993 of temperatures at the surface and in the troposphere were analyzed from radiosonde observations in eight north-latitude regions. The seasonal consistency of the surface and tropospheric trends of temperature and evening-morning temperature difference was examined for these regions. In most seasons the surface temperature trends were positive in Eurasia and western N. America but were negative in central N. America and eastern Canada. The regions with sizable and statistically significant surface temperature trends usually had significant tropospheric trends up to 500 mb and sometimes to 300 mb. An exception was central Asia, where the strong warming was confined below 850 mb. The significant tropospheric trends showed a tendency to de crease in magnitude with height. Trends of the evening minus morning temperature difference were also analyzed in two sectors, Canada and Russia, where the radiosonde launches occurred at 5am and pm +/-2hrs. Trends were fairly consistent in sign between the surface and lower troposphere in both sectors and up to 300 mb over Canada. Most Canadian trends were significant and represented a decreasing range between evening and morning temperatures. Significant Russian trends were primarily in summer. [References: 9]
机译:通过对八个北纬地区的探空仪观测,分析了1973-1993年21年期间地表和对流层温度的趋势。在这些区域检查了表面的季节一致性和对流层温度的趋势以及早晨的晚间温差。在大多数季节,欧亚大陆和北美西部的表面温度趋势为正,而北美中部和加拿大东部的表面温度趋势为负。具有相当大且具有统计意义的表面温度趋势的区域通常具有高达500 mb(有时甚至300 mb)的对流层趋势。中亚地区是个例外,那里的强烈变暖被限制在850 mb以下。对流层的显着趋势表明,随着高度的增加,其幅度会减小。还分析了加拿大和俄罗斯这两个部门的傍晚减去早晨温度差的趋势,其中无线电探空仪发射发生在凌晨5点和下午+/- 2小时。两个部门的对流层和低层对流层之间的趋势趋势基本一致,加拿大的最大对流层为300 mb。加拿大的大多数趋势都很明显,并且代表着夜间和早晨之间温度的递减范围。俄罗斯的主要趋势主要是在夏季。 [参考:9]

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