scholarly journals Estimation of colors of tree leaves with high vital power in northern urban area of Kyoto city

2003 ◽  
Vol 29 (1) ◽  
pp. 68-73
Author(s):  
Yuri SUZUKI ◽  
Shozo SHIBATA ◽  
Kazuhiro TANAKA ◽  
Tetsuro SAKAI
2006 ◽  
Vol 69 (5) ◽  
pp. 529-532 ◽  
Author(s):  
Hiroshi HASHIMOTO ◽  
Kuniyuki SAWA ◽  
Keizo TABATA ◽  
Yukihiro MORIMOTO ◽  
Shinya NISHIO
Keyword(s):  

2005 ◽  
Vol 10 (1) ◽  
pp. 25-35 ◽  
Author(s):  
Hiroshi Hashimoto ◽  
Kentaro Murakami ◽  
Yukihiro Morimoto

2003 ◽  
Vol 31 ◽  
pp. 387-394 ◽  
Author(s):  
Michinori Hatayama ◽  
Kyoko Terao ◽  
Yoshimi HAGIHARA ◽  
Kataya KANEYUKI

Chemosphere ◽  
2005 ◽  
Vol 61 (6) ◽  
pp. 753-760 ◽  
Author(s):  
M. Tomašević ◽  
Z. Vukmirović ◽  
S. Rajšić ◽  
M. Tasić ◽  
B. Stevanović

Radiocarbon ◽  
2017 ◽  
Vol 59 (3) ◽  
pp. 1009-1019 ◽  
Author(s):  
Maurice Ndeye ◽  
Matar Sène ◽  
Doudou Diop ◽  
Jean-François Saliège

AbstractRadiocarbon (14C) in atmospheric CO2 for the Dakar (Senegal) urban area was measured using tree leaves collected by botanists from 1900 to 2003. The aim of our study was to compare the local Suess effect in Dakar to the global one during the 20th century. The ∆14C of atmospheric CO2 in this region decreased from 1900 to 1958 during the pre-bomb era (–2±5‰ to –22±4‰). From 1958 to 1964, nuclear bomb tests injected a large amount of artificial 14C into the atmosphere, reflected in the rise of ∆14C values. In the Dakar region, the atmospheric ∆14C reached 773±8‰ in 1964, but subsequently decreased to 80±5‰ by 2003, which is consistent with the global exponential decreasing trend. The ∆14C record presented here remains slightly lower than the global record. This result is attributed to the input of anthropogenic fossil carbon into the atmosphere. The amount of carbon input can be evaluated by comparing urban areas to those of clean air sites. The calculation of anthropogenic fossil carbon is deduced from a simple mathematical model.


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