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| 1 | A Diagnostic Analysis on the Effect of the Residual Layer in Convective Boundary Layer Development near Mongolia Using 20th Century Reanalysis Data显示文摘Although the residual layer has already been noted in the classical diurnal cycle of the atmospheric boundary layer,its effect on the development of the convective boundary layer has not been well studied. In this study, based on 3-hourly20 th century reanalysis data, the residual layer is considered as a common layer capping the convective boundary layer. It is identified daily by investigating the development of the convective boundary layer. The region of interest is bounded by(30°–60° N, 80°–120° E), where a residual layer deeper than 2000 m has been reported using radiosondes. The lapse rate and wind shear within the residual layer are compared with the surface sensible heat flux by investigating their climatological means, interannual variations and daily variations. The lapse rate of the residual layer and the convective boundary layer depth correspond well in their seasonal variations and climatological mean patterns. On the interannual scale, the correlation coefficient between their regional averaged(40°–50°N, 90°–110° E) variations is higher than that between the surface sensible heat flux and convective boundary layer depth. On the daily scale, the correlation between the lapse rate and the convective boundary layer depth in most months is still statistically significant during 1970–2012. Therefore, we suggest that the existence of a deep neutral residual layer is crucial to the formation of a deep convective boundary layer near the Mongolian regions. | HAN Bo ZHAO Cailing L Shihua WANG Xin | 2015 | Advances in Atmospheric Sciences2015，32，6： | 5 |
| 2 | Different expression of alternative lengthening of telomere (ALT)-associated proteins/ mRNAs in osteosarcoma cell lines显示文摘 | ZHANG Y CAIL L WEIR X | 2011 | Oncology Letter2011，2，6： | 1 |
| 3 | Microsurgery and radiosurgery in brain arteriovenous malformations 显示文摘 | STEINER L LINDGUIST C CAIL W | 1993 | J Neurosurg1993，79，7： | 1 |
| 4 | Synthesis and structure-affinity relationships of new 4-(6-iodo-H-imidazo pyridin-2-yl)-N-dimethyl-benzeneamine derivatives as ligands for human a-amyloid plaques显示文摘 | Cail S Cuevas J Temme L | 2007 | J Med Chem2007，50，19： | 1 |
| 5 | Microsurgery and radio- surgery in brain arteriovenous malformations 显示文摘 | Stfiner L Lindquist C Cail W Steiner M | 1993 | J Neurosurg1993，79，5： | 1 |
| 6 | Cancer chemoprentive activity ofresveratrol, a natural product derived from grapes 显示文摘 | Jang M’Cail L Udeani GO | 1997 | Science1997，275，5297： | 1 |
| 7 | Global Land Surface Climate Analysis Based on the Calculation of a Modified Bowen Ratio显示文摘A modified Bowen ratio(BRm),the sign of which is determined by the direction of the surface sensible heat flux,was used to represent the major divisions in climate across the globe,and the usefulness of this approach was evaluated. Five reanalysis datasets and the results of an offline land surface model were investigated. We divided the global continents into five major BRm zones using the climatological means of the sensible and latent heat fluxes during the period 1980–2010:extremely cold,extremely wet,semi-wet,semi-arid and extremely arid. These zones had BRm ranges of(-∞,0),(0,0.5),(0.5,2),(2,10) and(10,+∞),respectively. The climatological mean distribution of the Bowen ratio zones corresponded well with the K ¨oppen-like climate classification,and it reflected well the seasonal variation for each subdivision of climate classification. The features of climate change over the mean climatological BRm zones were also investigated. In addition to giving a map-like classification of climate,the BRm also reflects temporal variations in different climatic zones based on land surface processes. An investigation of the coverage of the BRm zones showed that the extremely wet and extremely arid regions expanded,whereas a reduction in area was seen for the semi-wet and semi-arid regions in boreal spring during the period 1980–2010. This indicates that the arid regions may have become drier and the wet regions wetter over this period of time. | Bo HAN Shihua Lü Ruiqing LI Xin WANG Lin ZHAO Cailing ZHAO Danyun WANG Xianhong MENG | 2017 | Advances in Atmospheric Sciences2017，34，5： | 0 |
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