1) low cloud type
低云云型
2) typical low cloud region
典型低云区
1.
The data of wind fields and temperature fields from ERA40 and low cloud amount from ISCCP in July,2001 is used to analyze the relationship between cloud amount(hereafter,CA) and horizontal temperature advection(hereafter,HTA)at grid points in global typical low cloud regions(hereafter,GTLCRs)with conditional probability method(cloud frequency) and the daily evolution method.
选取欧洲中心40年再分析资料(ERA40)中2001年7月的775 hPa和925 hPa等压面上的风场和温度场资料与ISCCP同时段的低云资料,利用条件概率方法(云频数)和逐日演变的动态方法分析全球典型低云区单点的云量与水平温度平流的关系。
3) Low-level cloud
低云
1.
In order to understand the "Double ITCZ" in FGCM-0, this study first examines the low-level cloud cover and the bulk stability of the low troposphere over the eastern subtropical Pacific simulated by the National Center for Atmospheric Research (NCAR) Community Climate Model version 3 (CCM3), which is the atmosphere component model of FGCM-0.
为了认识FGCM-0中“双ITCZ”,首先研究了FGCM-0的大气分量模式,即NCAR(美国国家大气研究中心)的公用气候模式CCM3对秘鲁和加利福尼亚沿岸低云以及低层大气整体稳定度的模拟能力。
4) cloud type
云型
5) Low cloud amount
低云量
1.
Information of low cloud amount recorded in δ~(13)C series of tree ring cellulose of Pinus Koraiensis in Antu Area;
安图红松树轮稳定碳同位素记录的低云量信息
2.
According to the 13 stations records on air temperature, low cloud amount and sunshine time in each climatic belt and their relationship with global surface temperature (GST) during 1960-2007, the characteristics and principles of each climatic belt are analyzed.
其中南亚热带南区各个季节的增温速率都为最大;(4)低云量的年变化各气候带均呈上升趋势,其中中亚热带上升最明显;低云量与气温有明显的正相关;(5)日照的年变化各气候带均呈下降趋势,其中中亚热带下降最明显。
3.
Analysis on the complete correlation coefficients of climate factors with pan evaporation on regional average show that low cloud amount,average wind speed and diurnal temperature range were the main influencing factors resulted in pan evaporation decrease,but for different station they were different.
完全相关系数法分析表明,整个地区平均而言,低云量、平均风速、气温日较差与蒸发皿蒸发量有显著的相关性,是影响蒸发量的主要因子,但各站有所不同。
6) low cloud frequency
低云频数
补充资料：云云
【云云】
（杂语）言未尽之貌。止观辅行一之二曰：“云云者，未尽之貌。云者言也。说文，云象云气在天回转之形。言之在口，如云润物。广雅云：云者有也，下文尚有如云之言。”文句记一上曰：“云云者，象气之分散，如云在天，非可卒量也。意言下未说者，尚多如云。”
（杂语）言未尽之貌。止观辅行一之二曰：“云云者，未尽之貌。云者言也。说文，云象云气在天回转之形。言之在口，如云润物。广雅云：云者有也，下文尚有如云之言。”文句记一上曰：“云云者，象气之分散，如云在天，非可卒量也。意言下未说者，尚多如云。”
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条