Oyster mushroom is one of mushrooms that are cultivated and consumed a lot in Korea. P. ostreatus 'Suhan(ASI2504)' is a popluar cultivar because of high quality. But it is difficult for farmers to cultivate, so an alternative cultivar of ‘Suhan’ is demanded continuously. To develop a new variety, parental strains were selected using cultivation characteristics of Pleurotus ostreatus collected home and abroad. P. ostreatus 'Gosol' was developed by the method of Di-Mon crossing between dikaryotic strain P. ostreatus 'Mongdol(ASI0633)' and monokaryotic strain derived from P. ostreatus ‘Yasan(ASI0635)' in 2014. Analysis of the genetic characteristics of the new cultivar 'Gosol' showed a different DNA profile as that of the control strain, 'Suhan’ but a similar DNA profile as those of the parental strains, ‘Yasan’ and　'Mongdol’, when RAPD(Random Amplified Polymorphic DNA) primer URP 3 was used. The optimum temperature for mycelial growth was 25°C for ‘Gosol’ and ‘Suhan’. 'Gosol' was appropriate for middle high temperature to grow, especially 13~18°C. Fruiting body production per bottle was about 124.2g. When compared to the control strain 'Suhan’, the stipe was longer and the individual weight was heavier. But the stipe and the pileus were a little thinner than those of the control strain. ‘Gosol’ was more resistant at high CO2 concentration than the control strain. This new cultivar ‘Gosol’ of Pleurotus ostreatus was characterized dark bluish gray cultivar of oyster mushroom in the color of pileus and higer yield compared to those of other cultivar ‘Suhan’. Therefore, it is suggested that this new cultivar ‘Gosol’ be substitute for ‘Suhan’ in oyster mushroom’s farms.

A new commercial strain “Mongdol” of oyster mushroom was developed by hyphal anastomosis. It was improvedwith hybridization between monokaryotic strain derived from Pleurotus ostreatus ASI 0627 and dikaryotic strain derived from P.ostreatus ASI 2929. The optimum temperature of mycelial growth and fruiting body development were 25~30oC and 12~18oC,respectively. When two different media including PDA (potato dextrose agar medium) and MCM (mushroom complete medium)were compared, the mycelial growth of this mushroom was faster in MCM than in PDA. Similar result was observed with thecontrol strain P. ostreatus ASI 2504. Analysis of the genetic characteristics of the new cultivar “Mongdol” showed a different DNAprofile as that of the control strain ASI 2504, when RAPD (Random Amplified Polymorphic DNA) primer URP3 and URP6 wereused. Fruiting body production per bottle was about 106 g using demonstration farms. The color of pileus was blackish gray andthe stipe was long. Therefore, we expect that this new strain “Mongdol” will satisfy the consumer’s demand for high qualitymushrooms.

This study is carried out in order to bridge the gap to understand the relationships between South Asian and East Asian monsoon systems by comparing the summer (June-September) precipitation of Nepal and South Korea. Summer monsoon precipitation data from Nepal and South Korea during 30 years (1981-2010) are used in this research to investigate the association. NCEP/NCAR reanalysis data are also used to see the nature of large scale phenomena. Statistical applications are used to analyze these data. The analyzed results show that summer monsoon precipitation is higher over Nepal (1513.98 ± 159.29 mm y-1) than that of South Korea (907.80 ± 204.71 mm y-1) and the wettest period in both the countries is July. However, the coefficient of variation shows that amplitude of interannual variation of summer monsoon over South Korea (22.55%) is larger in comparison to that of Nepal (10.52%). Summer monsoon precipitation of Nepal is found to be significantly correlated to that of South Korea with a correlation coefficient of 0.52 (99% confidence level). Large-scale circulations are studied to further investigate the relationship between the two countries. wind and specific humidity at 850 hPa show a strong westerly from Arabian Sea to BOB and from BOB, wind moves towards Nepal in a northwestward direction during the positive rainfall years. In case of East Asia, strong northward displacement of wind can be observed from Pacific to South Korea and strong anticyclone over the northwestern Pacific Ocean. However, during the negative rainfall years, in the South Asian region we can find weak westerly from the Arabian Sea to BOB, wind is blowing in a southerly direction from Nepal and Bangladesh to BOB.