UFrankstar Mini Wave Buoy uhlinzeka ngokuxhaswa kwedatha okuqinile kososayensi baseChina ukutadisha ithonya le-SHANGHAI yomhlaba wonke endimeni yegagasi

UFranktar kanye nelebhu esemqoka ye-Oceregraphy engokomzimba, uMnyango Wezemfundo, i-Ocean University of China, ngokuhlangene i-Wave Sprites enyakatho-ntshonalanga yePacific Ocean kusukela kumanzi afanele afinyelela ezinsukwini ezifanele izinsuku ezingama-310. Ososayensi ebhularothri bahlaziywa ngokucophelela futhi basebenzisa idatha ye-Situ ebonwe ukufakazela ukuthi insimu yokugeleza kolwandle ingashintsha kakhulu izici zamagagasi olwandle. Leli phepha lokucwaninga lashicilelwa ePeep Sea Reports Party I, iphephabhuku eligunyaziwe embonini yasolwandle. Kubalulekile idatha yokubuka ye-SITU.

+ Ezinye

Le ndatshana ikhomba ukuthi kukhona imibono evuthiwe emhlabeni mayelana nethonya le-Ocean Currents emkhakheni Wave, osekelwa ngokwengeziwe ngochungechunge lwemiphumela yokulingiswa izinombolo. Kodwa-ke, ngokombono wokubona kwe-SITU, ubufakazi obanele nangobuphumelelayo awukanikezwanga ukwembula umphumela wokushintshana kwezintukuthelo zemisinga yolwandle kumagagasi, futhi sisantula ukuqonda okujulile komthelela we-Global-Scale ON Curres emasimini amagagasi.

Ngokuqhathanisa umehluko phakathi komkhiqizo we-wavewatch III Wave Model Model (GFS-WW3) kanye ne-In-Sive ebonwe ephakeme yama-wave buoys (ama-DRWBs), kuqinisekiswe endaweni yokubuka ukuthi imisipha yokubuka i-Ocean Curster ingakuthinta kakhulu i-Wave Heights. Ikakhulu, endaweni yaseKuroshio Extension Sealen yeNyakatho-ntshonalanga yePacific Ocean, lapho ukuqondiswa kokusakazeka kwe-Waves kufana (okuphambene) kuya endaweni yama-DRWBS, ephakeme) ukwedlula ukuhlolwa kwe-GFS-WW3. Ngaphandle kokubheka umphumela wokuphoqelela wamanje we-Ocean wapter on the wave field, umkhiqizo we-GFS-WW3 angaba nephutha elifinyelela ku-5% uma liqhathaniswa nokuphakama kwegagasi elisebenzayo elibonwa enkundleni. Ukuhlaziywa okwengeziwe kusetshenziswa ukubonwa kwe-satellite Altimeter kukhombisa ukuthi, ngaphandle kwezindawo zasolwandle eziphethwe yi-Ocean Slow (the Eastern-Latitude Ocean Product of GFS-WW3 Wave Production ngokuqondile kolwandle lwe-Global Ocean.

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Ukushicilelwa kwalesi sihloko kukhombisa ukuthi amapulatifomu okubukwa olwandle afuywayo kanye nezinzwa ezibukayo ezimelweI-Wave Buoykancane kancane wasondela futhi wafinyelela ezingeni lomhlaba wonke.

UFranktar uzokwenza eminye imizamo yokungaphenduli ukwethula amapulatifomu amaningi okubukwa kolwandle kanye nezinzwa, futhi enze okuthile aziqhenyayo!


Isikhathi sePosi: Oct-31-2022