1ON THE CAUSES OF RAINBAND BREAKING AND ASYMMETRIC PRECIPITATION IN TYPHOON HAITANG(2005) BEFORE AND AFTER ITS LANDFALLARTICLES513-520
2PRELIMINARY STUDY OF THE USE OF COSMIC DATA IN THE GLOBAL 3-DIMENSIONAL VARIANCE ASSIMILATION SYSTEM OF GRAPESARTICLES521-531
3EFFECTS OF AN ATMOSPHERIC COLD SOURCE OVER TIBETAN PLATEAU ON QUASI 4-YEAR OSCILLATION OF OCEAN-ATMOSPHERIC-LAND INTERACTIONSARTICLES532-540
4THE ROLE OF COLD AIR AND CHARACTERISTICS OF WATER VAPOR IN BOTH 0428 AND 7427 TYPHOONS THAT MADE LANDFALL ON CHINA IN WINTERTIMEARTICLES541-550
5ANALYSIS OF MESOSCALE CONVECTIVE SYSTEMS ASSOCIATED WITH A WARM SECTOR HEAVY RAINFALL EVENT OVER SOUTH CHINAARTICLES551-560
7STUDY ON THE EVOLVEMENT OF INITIAL ERRORS IN ENSEMBLE FORECAST OF HEAVY RAINS BASED ON BGMARTICLES571-575
9IMPACTS OF THE TROPICAL INDIAN-PACIFIC OCEAN THERMODYNAMIC ANOMALY JOINT MODE ON THE SUMMER RAINFALL OVER CHINAARTICLES581-588
11A SIMULATION EXPERIMENT ON OBSERVATION SYSTEM OF SINGULAR-VECTORS-BASED ADAPTIVE OBSERVATION FOR LOW PRESSURE ON THE MEI-YU FRONTARTICLES596-606
13THE RELATIONSHIP BETWEEN WINTERTIME BLOCKINGS IN THE NORTH HEMISPHERE AND NORTH ATLANTIC OSCILLATIONARTICLES615-620
15ANALYSIS OF MAINTAINING MECHANISMS OF PERSISTENT SEVERE HEAVY RAIN EVENTS IN SHANDONG PENINSULA FROM 10 TO 12 AUGUST 2007SHORT CONTRIBUTIONS628-634
16A CASE STUDY OF THE CHARACTERISTICS OF STRONG WIND NEAR THE OCEAN SURFACE DURING A STRONG COLD AIR PROCESS IN BOHE GUANGDONGSHORT CONTRIBUTIONS635-640
