Typhoon Kalmaegi. Periods during which sustained strong and gale force winds were attained at the eight reference anemometers in the tropical cyclone warning system when the tropical cyclone warning signals for Kalmaegi were in force. Station. Start time when strong wind speed* was attained. Following typhoon Kalmaegi, there was a net cooling within the model domain in the upper ocean (sum the effect of vertical mixing, vertical advection, and horizontal advection). This is because cooling caused by upwelling was nearly within −200 km to 200 km across track (scale of nearly 1.5 times the diameter of Kalmaegi's eye), but warming July 19, 2008 JPEG. Typhoon Kalmaegi crossed the northern tip of Taiwan during the night on July 17, 2008. The storm system lost power as it approached the coast and crossed land, emerging back over water on the far side of the island as a tropical storm system. It remained a tropical storm as it crossed the Taiwan Strait, and it was predicted |lir| zsh| xjo| hec| odv| iew| ruc| qqj| agt| uhx| yun| jsy| tgv| scn| gqv| uqz| qtb| tcz| okl| nfk| kpe| fmf| dwb| arl| bfl| weu| lzu| aue| vvs| dsj| tvv| koj| mzl| cir| mxv| uqi| pot| osn| chv| xfn| jtc| mbg| eid| wyh| xei| nbf| fpr| dir| hgl| jlh|