The Japanese Period in Indochina and the Coup of 9 March 1945

1978 ◽  
Vol 9 (2) ◽  
pp. 268-301 ◽  
Author(s):  
Ralph B. Smith

For the greater part of the period from 1940 to 1945, French Indochina occupied a peculiar place in the Co-Prosperity Sphere of Great East Asia. Following the capitulation of France before the German army in June 1940, the northern part of Indochina became the first area in Southeast Asia to admit Japanese troops — at that stage, as an extension of the Japanese campaign in southern China. In July 1941 the Japanese advance into southern Indochina marked the first step towards a full-scale attack on European and American possessions in the whole region, which materialized in December 1941. But this military advance into Indochina, precisely because it took place before the general assault on Southeast Asia and the Pacific, had to be achieved by means of agreements and treaties with an established government. These were possible only because the French in Indochina decided to recognize the pro-German government at Vichy, so that the Japanese were able to apply diplomatic pressure both in France and at Hanoi. Once the agreements had been made, the Japanese saw no need to change the basis of their occupation of Indochina even after December 1941; they were by then preoccupied with establishing their presence in other areas. Consequently they continued to recognize the French administration in Indochina and to maintain diplomatic relations with it, so long as diplomatic pressure was sufficient to ensure that Japanese military needs were fully met.

2012 ◽  
Vol 12 (9) ◽  
pp. 3837-3855 ◽  
Author(s):  
J. S. Fu ◽  
N. C. Hsu ◽  
Y. Gao ◽  
K. Huang ◽  
C. Li ◽  
...  

Abstract. To evaluate the impact of biomass burning from Southeast Asia to East Asia, this study conducted numerical simulations during NASA's 2006 Biomass-burning Aerosols in South-East Asia: Smoke Impact Assessment (BASE-ASIA). Two typical episode periods (27–28 March and 13–14 April) were examined. Two emission inventories, FLAMBE and GFED, were used in the simulations. The influences during two episodes in the source region (Southeast Asia) contributed to the surface CO, O3 and PM2.5 concentrations as high as 400 ppbv, 20 ppbv and 80 μg m−3, respectively. The perturbations with and without biomass burning of the above three species during the intense episodes were in the range of 10 to 60%, 10 to 20% and 30 to 70%, respectively. The impact due to long-range transport could spread over the southeastern parts of East Asia and could reach about 160 to 360 ppbv, 8 to 18 ppbv and 8 to 64 μg m−3 on CO, O3 and PM2.5, respectively; the percentage impact could reach 20 to 50% on CO, 10 to 30% on O3, and as high as 70% on PM2.5. In March, the impact of biomass burning mainly concentrated in Southeast Asia and southern China, while in April the impact becomes slightly broader and even could go up to the Yangtze River Delta region. Two cross-sections at 15° N and 20° N were used to compare the vertical flux of biomass burning. In the source region (Southeast Asia), CO, O3 and PM2.5 concentrations had a strong upward transport from surface to high altitudes. The eastward transport becomes strong from 2 to 8 km in the free troposphere. The subsidence process during the long-range transport contributed 60 to 70%, 20 to 50%, and 80% on CO, O3 and PM2.5, respectively to surface in the downwind area. The study reveals the significant impact of Southeastern Asia biomass burning on the air quality in both local and downwind areas, particularly during biomass burning episodes. This modeling study might provide constraints of lower limit. An additional study is underway for an active biomass burning year to obtain an upper limit and climate effects.


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