现代农业科技
現代農業科技
현대농업과기
XIANDAIHUA NONGYE
2014年
9期
259-262,264
,共5页
地面温度%变化趋势%河北沧州%1971-2010年
地麵溫度%變化趨勢%河北滄州%1971-2010年
지면온도%변화추세%하북창주%1971-2010년
ground temperature%change trend%Cangzhou Hebei%1971 to 2010
根据沧州市1971-2010年逐年、各季地温资料,采用差值法、折线图、气候变率等分析方法,对40年来沧州市地温变化趋势进行分析,发现沧州市近40年地面温度、地面最高温度、地面最低温度年平均值分别为14.8、29.3、6.5℃;地面温度四季气候变率只有秋季是降温趋势,各月气候变率、年气候变率均为上升趋势,近40年年代际变化呈波状变化;地面最高温度四季气候变率只有春季是升温趋势,各月气候变率为上升趋势,年气候变率为下降趋势,近40年年代际变化呈线性变化,总体下降趋势;地面最低温度四季气候变率均为升温趋势,以秋季升温速度最快,各月气候变率、年气候变率均为上升趋势,近40年年代际变化呈线性变化,总体呈上升趋势。
根據滄州市1971-2010年逐年、各季地溫資料,採用差值法、摺線圖、氣候變率等分析方法,對40年來滄州市地溫變化趨勢進行分析,髮現滄州市近40年地麵溫度、地麵最高溫度、地麵最低溫度年平均值分彆為14.8、29.3、6.5℃;地麵溫度四季氣候變率隻有鞦季是降溫趨勢,各月氣候變率、年氣候變率均為上升趨勢,近40年年代際變化呈波狀變化;地麵最高溫度四季氣候變率隻有春季是升溫趨勢,各月氣候變率為上升趨勢,年氣候變率為下降趨勢,近40年年代際變化呈線性變化,總體下降趨勢;地麵最低溫度四季氣候變率均為升溫趨勢,以鞦季升溫速度最快,各月氣候變率、年氣候變率均為上升趨勢,近40年年代際變化呈線性變化,總體呈上升趨勢。
근거창주시1971-2010년축년、각계지온자료,채용차치법、절선도、기후변솔등분석방법,대40년래창주시지온변화추세진행분석,발현창주시근40년지면온도、지면최고온도、지면최저온도년평균치분별위14.8、29.3、6.5℃;지면온도사계기후변솔지유추계시강온추세,각월기후변솔、년기후변솔균위상승추세,근40년년대제변화정파상변화;지면최고온도사계기후변솔지유춘계시승온추세,각월기후변솔위상승추세,년기후변솔위하강추세,근40년년대제변화정선성변화,총체하강추세;지면최저온도사계기후변솔균위승온추세,이추계승온속도최쾌,각월기후변솔、년기후변솔균위상승추세,근40년년대제변화정선성변화,총체정상승추세。
According to the data of mean ground temperature for all years and seasons in Cangzhou City from 1971 to 2010 ,using the difference method,line graph and climate change rate analysis method ,the ground temperature change trend during recent 40 years in Cangzhou City was analyzed.The result showed that the annual ground temperature ,annual ground highest and lowest temperature in Cangzhou City in recent 40 years were 14.8 ℃,29.3 ℃,6.5 ℃ respectively.Climate variability of ground temperature decreased in autumn ,the others showed rising trends.Interannual variation showed wavy distribution;Climate variability of the highest ground temperature increased in spring. The climate variability of each month showed an ascending trend ,the change rate showed a declined tendency in the last 40 years ,and interannual variation was a linear change;Climate variability of the lowest ground temperature increased ,and that of the autumn increased most significantly.The climate variability of each month and year both increased.Interannual variation was a linear change for 40 years ,and showed increasing trend in general.