[Early Online Release] Why did Northeast and Northwest China sometimes experience opposite winter temperature anomalies?
Citation: Yao, Y., and D.-H. Luo, 2014: The anomalous European climates linked to different Euro-Atlantic blocking, Atmos. Oceanic. Sci. Lett., 7, doi:10.3878/j.issn.1674-2834.14.0001.
http://159.226.119.58/aosl/EN/abstract/abstract458.shtml
Northeast and Northwest China sometimes experienced opposite winter temperature anomalies. What are their respective preceding factors?

Composite ((a)–(c))surface air temperature and ((d)–(f)) precipitation anomalies over the European continent averaged from lag(?2) to lag(+2) days for the blocking events over: ((a), (d)) Greenland, ((b), (e)) EAWE, and (c, f) east Europe. Thick solid (dotted) lines in the shaded area denote the positive (negative) anomaly region above the 99% confidence level for a two-sided Student’s t-test. The units of temperature (precipitation) anomaly are °C (mm). The correlation distribution of ((g)–(i)) the surface air temperature and ((j)–(l)) precipitation with winter mean blocking frequency time series for the blocking events over: ((g), (j)) Greenland, ((h), (k)) EAWE, and ((i), (l)) east Europe. The shaded area indicates the correlation coefficients above the 99% confidence level for a correlation test.
Northeast and Northwest China sometimes experienced opposite winter temperature anomalies. What are their respective preceding factors?