Journal of Tropical Oceanography ›› 2022, Vol. 41 ›› Issue (5): 17-28.doi: 10.11978/2021160CSTR: 32234.14.2021160
• Marine Meteorology • Previous Articles Next Articles
SHU Aiqing1(), XU Dongmei1,2,4(
), LI Hong2, WU Haiying3, SHEN Feifei1,2, DEND Hua1, BAI Yawen1
Received:
2021-11-16
Revised:
2022-01-11
Online:
2022-09-10
Published:
2022-01-17
Contact:
XU Dongmei
E-mail:20211201033@nuist.edu.cn;dmxu@nuist.edu.cn
Supported by:
CLC Number:
SHU Aiqing, XU Dongmei, LI Hong, WU Haiying, SHEN Feifei, DEND Hua, BAI Yawen. Assimilating MWHS-2 radiance of FY-3D satellite and its influence on the forecast of Typhoon Mitag*[J].Journal of Tropical Oceanography, 2022, 41(5): 17-28.
Tab. 1
The characterictics of each channel of MWHS-2"
通道 | 中心频率/GHz | 极化方式 | 带宽/MHz | 频率稳定度/MHz | 灵敏度/K | 主波束宽度/(°) | 主波束效率/% |
---|---|---|---|---|---|---|---|
1 | 89.0 | V | 1500 | 50 | 1.0 | 2.0 | >92 |
2 | 118.75±0.08 | H | 20 | 30 | 3.6 | 2.0 | >92 |
3 | 118.75±0.2 | H | 100 | 30 | 2.0 | 2.0 | >92 |
4 | 118.75±0.3 | H | 165 | 30 | 1.6 | 2.0 | >92 |
5 | 118.75±0.8 | H | 200 | 30 | 1.6 | 2.0 | >92 |
6 | 118.75±1.1 | H | 200 | 30 | 1.6 | 2.0 | >92 |
7 | 118.75±2.5 | H | 200 | 30 | 1.6 | 2.0 | >92 |
8 | 118.75±3.0 | H | 1000 | 30 | 1.0 | 2.0 | >92 |
9 | 118.75±5.0 | H | 2000 | 30 | 1.0 | 2.0 | >92 |
10 | 150.0 | V | 1500 | 50 | 1.0 | 1.1 | >95 |
11 | 183.31±1 | H | 500 | 30 | 1.0 | 1.1 | >95 |
12 | 183.31±1.8 | H | 700 | 30 | 1.0 | 1.1 | >95 |
13 | 183.31±3 | H | 1000 | 30 | 1.0 | 1.1 | >95 |
14 | 183.31±4.5 | H | 2000 | 30 | 1.0 | 1.1 | >95 |
15 | 183.31±7 | H | 2000 | 30 | 1.0 | 1.1 | >95 |
Fig. 5
Scatter plots of channel 11 brightness temperature background versus observation before bias correction (a, d), background versus observation after bias correction (b, e), analysis versus observation (c, f) after bias correction, at 06:00 UTC on 30th September 2019 (a, b, c) and at 18:00 UTC on 30th September 2019 (d, e, f)"
Fig. 7
500 hPa potential increment (units: gpm) of GTS_DA experiment (a), MWHS_DA experiment (b), the difference between MWHS_DA and GTS_DA experiment (c), the difference between ATMS_DA and GTS_DA experiment (d) at 06:00 UTC on 30th September 2019. The red typhoon symbol represents the observed location of typhoon"
Fig. 8
500 hPa temperature increment (units: K) of GTS_DA experiment (a), MWHS_DA experiment (b), the difference between MWHS_DA and GTS_DA experiment (c), the difference between ATMS_DA and GTS_DA experiment (d) at 06:00 UTC on 30th September 2019. The red typhoon symbol represents the observed location of typhoon"
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