Take-off time 9:12 am local (0012Z); flight duration 7.5 hours
Title: Warm conveyor belt and cyclonic recirculation Objectives: (1) to examine the "wrap-around" recirculation around a kamikaze cyclonic bomb NE of Japan; (2) to sample the warm conveyor belt ahead of a newer front pushed east from Japan (and responsible for snow over Yokota that morning); (3) to provide DIAL support to the ACE-Asia Twin Otter radiation experiment over the Sea of Japan north of Iwakuni.
Execution: The flight track was a "box" around Honshu and Hokkaido. We headed W to (35N, 131E) to overfly the Twin Otter on their wall between (35.5N, 131.8E) and (35.7N, 131.7E) at 0135-0138Z. We then headed NE to the northern tip of Hokkaido at (45N, 141E) followed by a SE leg to (39N, 150E) to sample the wrap-around circulation around the kamikaze cyclonic bomb that had been sitting to the NE of Hokkaido for the past few days. From there we flew SW to Yokota (36N, 139E), sampling the rising air along the warm conveyor belt pushed east of Japan.
Results: We met our objectives and sampled complicated chemical signatures associated with the warm conveyor belt and the cyclonic recirculation. Climbing out of Yokota we saw considerable fine structure below 10Kft associated with lifting of Japanese pollution by the front sitting over the area at the time, and coarser pollution structure above interwoven with stratospheric filaments (recirculation around the kamikaze?). The 31Kft leg to Iwakuni was in and out of the stratosphere. The Twin Otter overfly was conducted in a clear patch in a broken cloud field with good functioning of the DIAL. Heading NE over the Sea of Japan, we observed a depressed tropopause at 18Kft (jet stream), complicated pollution influences just below (the recirculation?) and direct Korean outflow below 10Kft with everything elevated (200-250 ppbv CO). As we approached the northern tip of Hokkaido the tropopause rose, and we sampled extensive aged (?) pollution at all altitudes (CO 150-200 ppbv, high PAN, C2Cl4, nitriles, moderately high SO2, HCHO, ). Heading back SE and then SW we observed a range of Asian outflow layers at all levels with different chemical signatures. The recirculating pollution in the north showed moderately high CO (150-200 ppb), high C2Cl4, PAN, nitriles, low HCHO, and was interleaved with stratospheric filaments. The warm conveyor belt further south showed higher CO (up to 300 ppb). NO was very low in the "recirculating pollution" (< 10 pptv) but had a lot of structure with values in excess of 100 pptv in the warm conveyor belt associated with recent convection (high CH3OOH/H2O2 ratios). The NO structure was probably associated at least in part with lightning.
Meteorological Summary Yokota Local # 5 31 March 2001
Flow Features:
Cloud Features and Other Goodies:
Stratospheric air was encountered during the southwestern part of the
flight track. This region was in the left entrance region of the jet
streak described above.