Atmospheric Circulation Patterns over East Asia and Their Connection with Summer Precipitation and Surface Air Temperature in Eastern China during 1961–2013

Shuping LI; Wei HOU; Guolin FENG

doi:10.1007/s13351-018-7071-4

PDF (12589 KB)

Atmospheric Circulation Patterns over East Asia and Their Connection with Summer Precipitation and Surface Air Temperature in Eastern China during 1961–2013

Shuping LI¹,
Wei HOU²,
Guolin FENG^1,2,3, ,

+ Author Affiliations + Find other works by these authors

Corresponding author: Guolin FENG, fenggl@cma.gov.cn;

Funds:

Supported by the National Natural Science Foundation of China (41530531, 41675092, and 41305056) and China Meteorological Administration Special Public Welfare Research Fund (GYHY201506001)

DOI: 10.1007/s13351-018-7071-4

Abstract

Abstract

Based on the NCEP/NCAR reanalysis data and Chinese observational data during 1961–2013, atmospheric circulation patterns over East Asia in summer and their connection with precipitation and surface air temperature in eastern China as well as associated external forcing are investigated. Three patterns of the atmospheric circulation are identified, all with quasi-barotropic structures: (1) the East Asia/Pacific (EAP) pattern, (2) the Baikal Lake/Okhotsk Sea (BLOS) pattern, and (3) the eastern China/northern Okhotsk Sea (ECNOS) pattern. The positive EAP pattern significantly increases precipitation over the Yangtze River valley and favors cooling north of the Yangtze River and warming south of the Yangtze River in summer. The warm sea surface temperature anomalies over the tropical Ind-ian Ocean suppress convection over the northwestern subtropical Pacific through the Ekman divergence induced by a Kelvin wave and excite the EAP pattern. The positive BLOS pattern is associated with below-average precipitation south of the Yangtze River and robust cooling over northeastern China. This pattern is triggered by anomalous spring sea ice concentration in the northern Barents Sea. The anomalous sea ice concentration contributes to a Rossby wave activity flux originating from the Greenland Sea, which propagates eastward to North Pacific. The positive ECNOS pattern leads to below-average precipitation and significant warming over northeastern China in summer. The reduced soil moisture associated with the earlier spring snowmelt enhances surface warming over Mongolia and northeastern China and the later spring snowmelt leads to surface cooling over Far East in summer, both of which are responsible for the formation of the ECNOS pattern.
- atmospheric circulation patterns,
- precipitation,
- surface air temperature,
- external forcing

FullText(HTML)

Fig. 1. Leading modes of the summer 500-hPa geopotential height anomalies over East Asia and their corresponding PCs: (a) EOF1, (b) EOF2, (c) EOF3, (d) PC1, (e) PC2, and (f) PC3. The numbers in blue at the top of the right-hand panels indicate the percentage of variance explained.

Download: Larger image PowerPoint slide

Fig. 2. Summer mean anomalies regressed onto PC1 for 1961–2013: (a) 200-, (b) 500-, and (c) 850-hPa geopotential height (gpm), and (d) SLP (hPa). The dotted areas exceed the 95% confidence level with a two-tailed Student’s t-test.

Download: Larger image PowerPoint slide

Fig. 3. As in Fig. 2, but for PC2.

Download: Larger image PowerPoint slide

Fig. 4. As in Fig. 2, but for PC3.

Download: Larger image PowerPoint slide

Fig. 5. Observed summer precipitation anomalies (mm) regressed onto (a) PC1, (c) PC2, and (e) PC3 for 1961–2013 and the spatial distribution of the explained variance of the (b) EAP, (d) BLOS and (f) ECNOS patterns. The black dots in (a, c, e) indicate areas exceeding the 95% confidence level with a two-tailed Student’s t-test.

Download: Larger image PowerPoint slide

Fig. 6. As in Fig. 5, but for the summer SAT (℃).

Download: Larger image PowerPoint slide

Fig. 7. Correlations between PC1 and seasonal mean SST in (a) the preceding winter, (b) spring, (c) summer, and (d) autumn. The dotted areas indicate the 95% confidence level with a two-tailed Student’s t-test.

Download: Larger image PowerPoint slide

Fig. 8. Summer mean (a) SST (shading; ℃), (b) 300-hPa potential velocity (contours; m² s^–1) and divergent wind (vectors; m s^–1), and (c) 300-hPa geopotential height (shading; gpm) and 850-hPa horizontal wind (vectors; m s^–1) anomalies associated with the simultaneous TIO index for 1961–2013. (d)–(f) Same as (a)–(c), respectively, but associated with PC1. In (a, d), the green solid lines indicate the 27.5℃ of the total SST associated with the TIO index and PC1, respectively. The total SST is defined as the sum of the TIO index/PC1 regression pattern and climatological mean SST. In (b, e), the contour interval is 0.1 × 10⁵ m² s^–1; the zero contour lines are black, whereas the negative (positive) values are blue (red).

Download: Larger image PowerPoint slide

Fig. 9. Summer mean (a) net latent heat flux (shading; W m^–2) and 10-m wind (vectors; m s^–1), (b) outgoing longwave radiation (W m^–2), (c) 500-hPa vertical velocity (Pa s^–1), and (d) precipitation (mm day^–1) anomalies associated with the simultaneous TIO index. The dotted areas exceed the 95% confidence level with a two-tailed Student’s t-test.

Download: Larger image PowerPoint slide

Fig. 10. Correlation between PC2 and seasonal mean SIC in (a) the preceding winter and (b) spring. The dotted areas exceed the 95% confidence level with a two-tailed Student’s t-test.

Download: Larger image PowerPoint slide

Fig. 11. (a) Spring mean SIC and (b) summer mean 300-hPa geopotentail height (shading; gpm) and wave activity flux (vectors; m^–2 s^–2) anomalies associated with the inverted SSIC index. (c, d) Same as (a, b), but are associated with PC2. The dotted areas indicate the 95% confidence level with a two-tailed Student’s t-test.

Download: Larger image PowerPoint slide

Fig. 12. Spring mean (a) SLP, (b) SST (shading; °C) and 10-m wind (vectors; m s^–1) anomalies regressed onto PC2, summer mean (c) SST (shading) and 10-m wind (vectors), and (d) precipitation (shading; mm day^–1) and divergent wind anomalies (vectors; m s^–1) regressed onto the spring Victoria mode index. The Victoria mode index is defined as the normalized PC of the second EOF mode of the North Pacific SST anomalies in spring. The dotted areas exceed the 95% confidence level with a two-tailed Student’s t-test.

Download: Larger image PowerPoint slide

Fig. 13. Correlation between PC3 and SCE in (a) spring, (b) April, (c) May, and (d) June during 1973–2013.The dotted areas exceed the 90% confidence level with a two-tailed Student’s t-test.

Download: Larger image PowerPoint slide

Fig. 14. Summer mean (a) 0–10-cm soil moisture (m³ m^–3) and (b) 2-m air temperature anomalies (℃) regressed onto the spring snowmelt index. The dotted areas indicate the 95% confidence level with a two-tailed Student’s t-test.

Download: Larger image PowerPoint slide

Table 1 Correlation coefficients between the BLOS and ECNOS patterns and the conventional atmospheric circulation teleconnection patterns in the Northern Hemisphere. The symbols * and ** indicate the 90% and 95% confidence level, respectively

Pattern	AO	NAO	POL	EA	WA	EU	SCAN	EAWR	WP
BLOS	–0.096	0.341^**	–0.273^**	–0.169	–0.031	–0.127	–0.282^**	0.311^**	–0.025
ECNOS	0.209	0.076	0.221	0.236^*	–0.052	–0.197	–0.082	0.070	0.234^*

Download: Download as CSV

References (60)

References

Betts, A. K., 2007: Coupling of water vapor convergence, clouds, precipitation, and land-surface processes. J. Geophys. Res., 112, D10108. doi: 10.1029/2006JD008191

Bond, N. A., J. E. Overland, M. Spillane, et al., 2003: Recent shifts in the state of the North Pacific. Geophys. Res. Lett., 30, 2183. doi: 10.1029/2003GL018597

Chen, M. Y., P. P. Xie, J. E. Janowiak, et al., 2002: Global land precipitation: A 50-yr monthly analysis based on gauge observations. J. Hydrometeor., 3, 249–266. doi: 10.1175/1525-7541(2002)003<0249:GLPAYM>2.0.CO;2

Chen, S. F., and R. G. Wu, 2017: Interdecadal changes in the relationship between interannual variations of spring North Atlantic SST and Eurasian surface air temperature. J. Climate, 30, 3771–3787. doi: 10.1175/JCLI-D-16-0477.1

Chen, Y., and P. M. Zhai, 2015: Synoptic-scale precursors of the East Asia/Pacific teleconnection pattern responsible for persistent extreme precipitation in the Yangtze River valley. Quart. J. Roy. Meteor. Soc., 141, 1389–1403. doi: 10.1002/qj.2448

Comiso, J. C., C. L. Parkinson, R. Gersten, et al., 2008: Accelerated decline in the Arctic sea ice cover. Geophys. Res. Lett., 35, L01703. doi: 10.1029/2007GL031972

Derksen, C., and R. Brown, 2012: Spring snow cover extent reductions in the 2008–2012 period exceeding climate model projections. Geophys. Res. Lett., 39, L19504. doi: 10.1029/2012GL053387

Diao, Y. N., S. P. Xie, and D. H. Luo, 2015: Asymmetry of winter European surface air temperature extremes and the North Atlantic oscillation. J. Climate, 28, 517–530. doi: 10.1175/JCLI-D-13-00642.1

Ding, R. Q., K. J. Ha, and J. P. Li, 2010: Interdecadal shift in the relationship between the East Asian summer monsoon and the tropical Indian Ocean. Climate Dyn., 34, 1059–1071. doi: 10.1007/s00382-009-0555-2

Ding, R. Q., J. P. Li, Y. H. Tseng, et al., 2015a: The Victoria mode in the North Pacific linking extratropical sea level pressure variations to ENSO. J. Geophys. Res., 120, 27–45. doi: 10.1002/2014JD022221

Ding, R. Q., J. P. Li, Y. H. Tseng, et al., 2015b: Influence of the North Pacific Victoria mode on the Pacific ITCZ summer precipitation. J. Geophys. Res., 120, 964–979. doi: 10.1002/2014JD022364

Ding, R. Q., J. P. Li, Y. H. Tseng, et al., 2016: Interdecadal change in the lagged relationship between the Pacific–South Ameri-can pattern and ENSO. Climate Dyn., 47, 2867–2884. doi: 10.1007/s00382-016-3002-1

Ding, Y. H., 1992: Summer monsoon rainfalls in China. J. Meteor. Soc. Japan Ser. II, 70, 373–396. doi: 10.2151/jmsj1965.70.1B_373

Feng, J., W. Chen, and Y. J. Li, 2017: Asymmetry of the winter extra-tropical teleconnections in the Northern Hemisphere associated with two types of ENSO. Climate Dyn., 48, 2135–2151. doi: 10.1007/s00382-016-3196-2

Gong, D. Y., and C. H. Ho, 2002: Shift in the summer rainfall over the Yangtze River valley in the late 1970s. Geophys. Res. Lett., 29, 1436. doi: 10.1029/2001gl014523

Graham, N. E., and T. P. Barnett, 1987: Sea surface temperature, surface wind divergence, and convection over tropical oceans. Science, 238, 657–659. doi: 10.1126/science.238.4827.657

Groisman, P. Y., R. W. Knight, V. N. Razuvaev, et al., 2006: State of the ground: Climatology and changes during the past 69 years over northern Eurasia for a rarely used measure of snow cover and frozen land. J. Climate, 19, 4933–4955. doi: 10.1175/JCLI3925.1

Honda, M., K. Yamazaki, Y. Tachibana, et al., 1996: Influence of Okhotsk sea-ice extent on atmospheric circulation. Geophys. Res. Lett., 23, 3595–3598. doi: 10.1029/96GL03474

Huang, R. H., 1992: The East Asia/Pacific pattern teleconnection of summer circulation and climate anomaly in East Asia. Acta Meteor. Sinica, 6, 25–37.

Huang, R. H., and J. L. Chen, 2010: Characteristics of the summertime water vapor transports over the eastern part of China and those over the western part of China and their difference. Chinese J. Atmos. Sci., 34, 1035–1045. (in Chinese)

Huang, S. S., and M. M. Tang, 1987: On the structure of the summer monsoon regime of East Asia. Scientia Meteorologica Sinica, 8, 1–14. (in Chinese)

Jiang, T., Z. W. Kundzewicz, and B. D. Su, 2008: Changes in monthly precipitation and flood hazard in the Yangtze River basin, China. Int. J. Climatol., 28, 1471–1481. doi: 10.1002/joc.1635

Kalnay, E., M. Kanamitsu, R. Kistler, et al., 1996: The NCEP/NCAR 40-year reanalysis project. Bull. Amer. Meteor. Soc., 77, 437–471. doi: 10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO;2

Li, J. P., J. Feng, and Y. Li, 2012: A possible cause of decreasing summer rainfall in northeast Australia. Int. J. Climatol., 32, 995–1005. doi: 10.1002/joc.2328

Li, X. Z., W. Zhou, D. L. Chen, et al., 2014: Water vapor transport and moisture budget over eastern China: Remote forcing from the two types of El Niño. J. Climate, 27, 8778–8792. doi: 10.1175/JCLI-D-14-00049.1

Li, Y. F., and L. R. Leung, 2013: Potential impacts of the Arctic on interannual and interdecadal summer precipitation over China. J. Climate, 26, 899–917. doi: 10.1175/JCLI-D-12-00075.1

Liebmann, B., and C. A. Smith, 1996: Description of a complete (interpolated) outgoing longwave radiation dataset. Bull. Amer. Meteor. Soc., 77, 1275–1277.

Luo, B. H., and Y. Yao, 2018: Recent rapid decline of the Arctic winter sea ice in Barents–Kara Seas owing to combined Ural Blocking and SST. J. Meteor. Res., 32, 191–202. doi: 10.1007/s13351-018-7104-z

Matsumura, S., K. Yamazaki, and T. Tokioka, 2010: Summertime land-atmosphere interactions in response to anomalous springtime snow cover in northern Eurasia. J. Geophys. Res., 115, D20107. doi: 10.1029/2009JD012342

Matsumura, S., and K. Yamazaki, 2012: Eurasian subarctic summer climate in response to anomalous snow cover. J. Climate, 25, 1305–1317. doi: 10.1175/2011JCLI4116.1

Ninomiya, K., and H. Mizuno, 1985: Anomalous cold spell in summer over northeastern Japan caused by northeasterly wind from polar maritime airmass. Part 1: EOF analysis of temperature variation in relation to the large-scale situation causing the cold summer. J. Meteor. Soc. Japan, 63, 845–857. doi: 10.2151/jmsj1965.63.5_845

Nitta, T., 1987: Convective activities in the tropical western Pacific and their impact on the Northern Hemisphere summer circulation. J. Meteor. Soc. Japan, 65, 373–390. doi: 10.2151/jmsj1965.65.3_373

Notaro, M., W. C. Wang, and W. Gong, 2006: Model and observational analysis of the Northeast U.S. regional climate and its relationship to the PNA and NAO patterns during early winter. Mon. Wea. Rev., 134, 3479–3505. doi: 10.1175/MWR3234.1

Park, T. W., C. H. Ho, and S. Yang, 2011: Relationship between the Arctic oscillation and cold surges over East Asia. J. Climate, 24, 68–83. doi: 10.1175/2010JCLI3529.1

Qu, X., and G. Huang, 2012: Impacts of tropical Indian Ocean SST on the meridional displacement of East Asian jet in boreal summer. Int. J. Climatol., 32, 2073–2080. doi: 10.1002/joc.2378

Rayner, N. A., D. E. Parker, E. B. Horton, et al., 2003: Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century. J. Geophys. Res., 108, 4407. doi: 10.1029/2002JD002670

Robinson, D. A., K. F. Dewey, and R. R. Heim Jr, 1993: Global snow cover monitoring: An update. Bull. Amer. Meteor. Soc., 74, 1689–1696. doi: 10.1175/1520-0477(1993)074<1689:GSCMAU>2.0.CO;2

Shi, N., and Q. G. Zhu, 1996: An abrupt change in the intensity of the East Asian summer monsoon index and its relationship with temperature and precipitation over East China. Int. J. Climatol., 16, 757–764. doi: 10.1002/(SICI)1097-0088(199607)16:7<757::AID-JOC50>3.0.CO;2-5

Smith, T. M., R. W. Reynolds, T. C. Peterson, et al., 2008: Improvements to NOAA’s historical merged land–ocean surface temperature analysis (1880–2006). J. Climate, 21, 2283–2296. doi: 10.1175/2007JCLI2100.1

Sun, C., J. P. Li, F. F. Jin, et al., 2013: Sea surface temperature inter-hemispheric dipole and its relation to tropical precipitation. Environ. Res. Lett., 8, 044006. doi: 10.1088/1748-9326/8/4/044006

Sung, M. K., W. T. Kwon, H. J. Baek, et al., 2006: A possible impact of the North Atlantic oscillation on the East Asian summer monsoon precipitation. Geophys. Res. Lett., 33, L21713. doi: 10.1029/2006GL027253

Takaya, K., and H. Nakamura, 2001: A formulation of a phase-independent wave-activity flux for stationary and migratory quasigeostrophic eddies on a zonally varying basic flow. J. Atmos. Sci., 58, 608–627. doi: 10.1175/1520-0469(2001)058<0608:AFOAPI>2.0.CO;2

Tao, S. Y., and L. X. Chen, 1987: A review of recent research on the East Asian summer monsoon in China. Monsoon Meteorology. C. P. Chang and T. N. Krishnamurti, Eds., Oxford University Press, New York, 353 pp.

Trenberth, K. E., and J. M. Caron, 2000: The Southern Oscillation revisited: Sea level pressures, surface temperatures, and precipitation. J. Climate, 13, 4358–4365. doi: 10.1175/1520-0442(2000)013<4358:TSORSL>2.0.CO;2

Wallace, J. M., and D. S. Gutzler, 1981: Teleconnections in the geopotential height field during the Northern Hemisphere winter. Mon. Wea. Rev., 109, 784–812. doi: 10.1175/1520-0493(1981)109<0784:TITGHF>2.0.CO;2

Wang, J. B., Z. P. Wen, R. G. Wu, et al., 2016: The mechanism of growth of the low-frequency East Asia–Pacific teleconnection and the triggering role of tropical intraseasonal oscillation. Climate Dyn., 46, 3965–3977. doi: 10.1007/s00382-015-2815-7

Wang, S. S., J. P. Huang, Y. L. He, et al., 2014: Combined effects of the Pacific decadal oscillation and El Niño–Southern oscillation on global land dry–wet changes. Sci. Rep., 4, 6651. doi: 10.1038/srep06651

Wang, W. W., W. Zhou, X. Z. Li, et al., 2016: Synoptic-scale characteristics and atmospheric controls of summer heat waves in China. Climate Dyn., 46, 2923–2941. doi: 10.1007/s00382-015-2741-8

Wu, B. Y., R. H. Zhang, and B. Wang, 2009: On the association between spring Arctic sea ice concentration and Chinese summer rainfall: A further study. Adv. Atmos. Sci., 26, 666–678. doi: 10.1029/2009GL037299

Wu, B. Y., R. H. Zhang, R. D’Arrigo, et al., 2013: On the relationship between winter sea ice and summer atmospheric circulation over Eurasia. J. Climate, 26, 5523–5536. doi: 10.1175/JCLI-D-12-00524.1

Wu, R. G., and B. P. Kirtman, 2007: Observed relationship of spring and summer East Asian rainfall with winter and spring Eurasian snow. J. Climate, 20, 1285–1304. doi: 10.1175/JCLI4068.1

Wu, Z. W., J. P. Li, Z. H. Jiang, et al., 2012: Possible effects of the North Atlantic oscillation on the strengthening relationship between the East Asian summer monsoon and ENSO. Int. J. Climatol., 32, 794–800. doi: 10.1002/joc.2309

Xie, S. P., and S. G. H. Philander, 1994: A coupled ocean–atmosphere model of relevance to the ITCZ in the eastern Pacific. Tellus A, 46, 340–350. doi: 10.1034/j.1600-0870.1994.t01-1-00001.x

Xie, S. P., K. M. Hu, J. Hafner, et al., 2009: Indian Ocean capacitoreffect on Indo-western Pacific climate during the summer following El Niño. J. Climate, 22, 730–747. doi: 10.1175/2008JCLI2544.1

Zhang, L., and T. Li, 2017: Physical processes responsible for the interannual variability of sea ice concentration in Arctic in boreal autumn since 1979. J. Meteor. Res., 31, 468–475. doi: 10.1007/s13351-017-6105-7

Zhang, Q. Y., and S. Y. Tao, 1998: Influence of Asian mid-high latitude circulation on east Asian summer rainfall. Acta Meteor. Sinica, 56, 199–211. (in Chinese) doi: 10.11676/qxxb1998.019.

Zhang, R. N., R. H. Zhang, and Z. Y. Zuo, 2017: Impact of Eurasianspring snow decrement on East Asian summer precipitation. J. Climate, 30, 3421–3437. doi: 10.1175/JCLI-D-16-0214.1

Zhao, P., Y. N. Zhu, and R. H. Zhang, 2007: An Asian–Pacific teleconnection in summer tropospheric temperature and associated Asian climate variability. Climate Dyn., 29, 293–303. doi: 10.1007/s00382-007-0236-y

Zheng, F., J. P. Li, R. T. Clark, et al., 2013: Simulation and projection of the Southern Hemisphere annular mode in CMIP5 models. J. Climate, 26, 9860–9879. doi: 10.1175/JCLI-D-13-00204.1

Zheng, J. Y., J. P. Li, and J. Feng, 2014: A dipole pattern in the Indian and Pacific oceans and its relationship with the East Asiansummer monsoon. Environ. Res. Lett., 9, 074006. doi: 10.1088/1748-9326/9/7/074006

Relative Articles

Supplements (0)

Cited By

Cited by

Periodical cited type(18)

1.	Muhammad Waqas, Usa Wannasingha Humphries, Phyo Thandar Hlaing, et al. Seasonal WaveNet-LSTM: A Deep Learning Framework for Precipitation Forecasting with Integrated Large Scale Climate Drivers. Water, 2024, 16(22): 3194. DOI:10.3390/w16223194
2.	Shuping Li, Guolin Feng, Pengcheng Yan, et al. Relationship between Summer Synoptic Circulation Patterns and Extreme Precipitation in Northern China. Atmosphere, 2023, 14(12): 1705. DOI:10.3390/atmos14121705
3.	Muyuan Li, Jinfeng Yao, Yanbo Shen, et al. Impact of synoptic circulation patterns on renewable energy-related variables over China. Renewable Energy, 2023, 215: 118875. DOI:10.1016/j.renene.2023.05.133
4.	Huidi Yang, Jian Rao, Haohan Chen, et al. Lagged Linkage between the Kara–Barents Sea Ice and Early Summer Rainfall in Eastern China in Chinese CMIP6 Models. Remote Sensing, 2023, 15(8): 2111. DOI:10.3390/rs15082111
5.	Shuping Li, Tao Su, Pengcheng Yan, et al. The role of SST forcing in the interdecadal variations of the Pacific‐Japan pattern in the late 1990s. International Journal of Climatology, 2023, 43(3): 1514. DOI:10.1002/joc.7930
6.	Shibo Yao, Xianmei Lang, Dong Si, et al. Moisture sources of summer heavy precipitation in two spatial patterns over Northeast China during 1979–2021. Atmospheric Science Letters, 2023, 24(11) DOI:10.1002/asl.1181
7.	Kuo Wang, Zhihang Xu, Gaofeng Fan, et al. A Comprehensive Evaluation Model for Local Summer Climate Suitability under Global Warming: A Case Study in Zhejiang Province. Atmosphere, 2022, 13(7): 1075. DOI:10.3390/atmos13071075
8.	Weixing Zhao, Jieming Chou, Jiangnan Li, et al. Impacts of Extreme Climate Events on Future Rice Yields in Global Major Rice-Producing Regions. International Journal of Environmental Research and Public Health, 2022, 19(8): 4437. DOI:10.3390/ijerph19084437
9.	Yushan Zhang, Kun Wu, Jinglin Zhang, et al. Estimating Rainfall with Multi-Resource Data over East Asia Based on Machine Learning. Remote Sensing, 2021, 13(16): 3332. DOI:10.3390/rs13163332
10.	S Swetha, Jasti S Chowdary, Anant Parekh, et al. Decadal prediction skill for spring and summer surface air-temperature over India and its association with SST patterns in CFSv2 and CNRM coupled models. Journal of Earth System Science, 2021, 130(1) DOI:10.1007/s12040-021-01563-9
11.	Haixia Dai, Ke Fan. An effective downscaling model for operational prediction of summer precipitation over China. Atmospheric Research, 2021, 257: 105621. DOI:10.1016/j.atmosres.2021.105621
12.	Xiaoqing Ma, Zhicong Yin. Dipole pattern of summer ozone pollution in the east of China and its connection with climate variability. Atmospheric Chemistry and Physics, 2021, 21(21): 16349. DOI:10.5194/acp-21-16349-2021
13.	Siyuan Sun, Zhaoyong Guan, Dechao Ye. Summer Regional Daily‐Precipitation Extreme Events in Huang‐Huai Rivers Region of China and Their Relationships With Rossby Wave Packet Activities. Journal of Geophysical Research: Atmospheres, 2021, 126(7) DOI:10.1029/2020JD034065
14.	Bingjun Liu, Xuezhi Tan, Thian Y. Gan, et al. Global atmospheric moisture transport associated with precipitation extremes: Mechanisms and climate change impacts. WIREs Water, 2020, 7(2) DOI:10.1002/wat2.1412
15.	O. P. Osipova, E. Yu. Osipov. Atmospheric Circulation Processes and Precipitation Regime in the Northern Part of the Baikal Mountain Region. Russian Meteorology and Hydrology, 2019, 44(10): 695. DOI:10.3103/S106837391910008X
16.	Yeon-Woo Choi, Joong-Bae Ahn. Possible mechanisms for the coupling between late spring sea surface temperature anomalies over tropical Atlantic and East Asian summer monsoon. Climate Dynamics, 2019, 53(11): 6995. DOI:10.1007/s00382-019-04970-3
17.	Shiling Chen, Bingjun Liu, Xuezhi Tan, et al. Characteristics and circulation background of extreme precipitation over East China. Natural Hazards, 2019, 99(1): 537. DOI:10.1007/s11069-019-03758-2
18.	Shuping Li, Wei Hou, Guolin Feng. Corrigendum. Journal of Meteorological Research, 2018, 32(4): 670. DOI:10.1007/s13351-018-8777-z

Other cited types(0)

Search

Citation

Li, S. P., W. Hou, and G. L. Feng, 2018: Atmospheric circulation patterns over East Asia and their connection with summer precipitation and surface air temperature in eastern China during 1961–2013. J. Meteor. Res., 32(2), 203–218, doi: 10.1007/s13351-018-7071-4..

Citation:

Export: BibTex EndNote

Article Metrics

Article views: 814
PDF downloads: 25 Cited by: 18

Manuscript History

Received: 31 May 2017

Accepted: 06 December 2017

Final form: 31 March 2018

Published online: 26 April 2018

	Hua ZHANG, Fei WANG, Jian LI, Yihong DUAN, Congwen ZHU, Jingyi HE. 2022: Potential Impact of Tonga Volcano Eruption on Global Mean Surface Air Temperature. Journal of Meteorological Research, 36(1): 1-5. DOI: 10.1007/s13351-022-2013-6
	Yaohui LI, Cailing ZHAO, Tiejun ZHANG, Wei WANG, Haixia DUAN, Yuanpu LIU, Yulong REN, Zhaoxia PU. 2018: Impacts of Land-Use Data on the Simulation of Surface Air Temperature in Northwest China. Journal of Meteorological Research, 32(6): 896-908. DOI: 10.1007/s13351-018-7151-5
	Guirong TAN, Hong-Li REN, Haishan CHEN, Qinglong YOU. 2017: Detecting Primary Precursors of January Surface Air Temperature Anomalies in China. Journal of Meteorological Research, 31(6): 1096-1108. DOI: 10.1007/s13351-017-7013-6
	Rui WANG, Yunfei FU. 2017: Structural Characteristics of Atmospheric Temperature and Humidity inside Clouds of Convective and Stratiform Precipitation in the Rainy Season over East Asia. Journal of Meteorological Research, 31(5): 890-905. DOI: 10.1007/s13351-017-7038-x
	Yi SHI, Zhihong JIANG, Liangpeng DONG, Suhung SHEN. 2017: Statistical Estimation of High-Resolution Surface Air Temperature from MODIS over the Yangtze River Delta, China. Journal of Meteorological Research, 31(2): 448-454. DOI: 10.1007/s13351-017-6073-y
	Wei HUA, Guangzhou FAN, Yiwei ZHANG, Lihua ZHU, Xiaohang WEN, Yongli ZHANG, Xin LAI, Binyun WANG, Mingjun ZHANG, Yao HU, Qiuyue WU. 2017: Trends and Uncertainties in Surface Air Temperature over the Tibetan Plateau, 1951–2013. Journal of Meteorological Research, 31(2): 420-430. DOI: 10.1007/s13351-017-6013-x
	Senfeng LIU, Anmin DUAN. 2017: Impacts of the Leading Modes of Tropical Indian Ocean Sea Surface Temperature Anomaly on Sub-Seasonal Evolution of the Circulation and Rainfall over East Asia during Boreal Spring and Summer. Journal of Meteorological Research, 31(1): 171-186. DOI: 10.1007/s13351-016-6093-z
	YU Yong, NIU Shengjie, ZHANG Hua, WU Ziyue. 2013: Regional Climate Effects of Internally and Externally Mixed Aerosols over China. Journal of Meteorological Research, 27(1): 110-118. DOI: 10.1007/s13351-013-0111-1
	GU Yajin, WANG Hongli, LIU Jian. 2010: Latitude-Dependent Response of East Asian Summer Monsoon to External Forcing in the Last Millennium. Journal of Meteorological Research, 24(6): 671-679.
	Li Jianping, Chou Jifan. 1997: THE EFFECTS OF EXTERNAL FORCING,DISSIPATION AND NONLINEARITY ON THE SOLUTIONS OF ATMOSPHERIC EQUATIONS^*. Journal of Meteorological Research, 11(1): 57-65.

Atmospheric Circulation Patterns over East Asia and Their Connection with Summer Precipitation and Surface Air Temperature in Eastern China during 1961–2013