Isatellite iya kunceda ukuxela kwangaphambili ukuqhuma kwentaba-mlilo

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Isatellite iya kunceda ukuxela kwangaphambili ukuqhuma kwentaba-mlilo 20025_1
Isatellite iya kunceda ukuxela kwangaphambili ukuqhuma kwentaba-mlilo

Njengokuvela kwesi sifo, kusoloko kunokwenzeka ukuba kuqikelele iimpawu zokuqala kunye nokuqhushumba kwentaba-mlilo zihlala zilawula ukuqikelela kwangaphambili. Ngenxa yoku, protheces ezinokubakho ezinokubakho phantsi kokubeka esweni rhoqo, kunye nezixhobo ezibuthathaka zirekhoda intshukumo ye-crust, yothuthu olubuthathaka, iinguqu kwi-Gases ezivuza emoyeni. Nangona kunjalo, ezi mpawu azisoloko zibangelwa, ngoko inyani kwaye imeko ayikuqhubeki ngokupheleleyo kuqhubeka ngokungalindelekanga.

Indlela entsha yokuqikelela kokuqhushumba ifumene iQela laseTarrilo Girona (i-Tárilor isuka elabhorari ye-jet motions (JPL) NASA. Kwinqaku elipapashwe kwi-geosciengel ye-geoscieredel, banikezela ukubhekisa kumathuba espacecraft esele besebenza kwi-orbit ekufutshane. Iintaba-mvume ezinjalo ziyakwazi ukulandela umkhondo we-gormal yentaba-mlilo evela kwintaba-mlilo "ye-"SOORY 'intaba-mlilo epheleleyo kwaye iqaphela ukuba yindawo yokufudumeza eyingozi, enokusebenza njengomgcini wezaqhwithi.

Isatellite iya kunceda ukuxela kwangaphambili ukuqhuma kwentaba-mlilo 20025_2
I-Geoscience yendalo, DoI: 10.1038 / S41561-021-005050

Ukubonisa amandla ale ndlela, ababhali basebenzise idatha yokubeka esweni eqokelelwe yi-NASA TRARRA kunye ne-AQUA. Ngokudibeneyo bahlola umphezulu womhlaba kabini ngemini, enesigqibo malunga ne-1 x 1 yeekhilomitha. Ukusukela oko ukumiliselwa kwabo, ngo-2002, bekukho ukuqhushumba kwezihlanu okukhulu, ukungabali intaba-mlilo kwiziqithi ezincinci, imilinganiselo yobushushu engekho lula. Le yintaba-mlilo yaseJapan ontakwa, New Zealand Rupeju, iChile yaseChiledo, inkungu kwi-Cape Verde kwaye inciphise iAlaska.

Emva kokuvavanywa kwedatha yokuqwalaselwa kwesatellite yezi ntaba-mlilo, izazinzulu zifumanise ukuba iqondo lokushisa laqala ngokuthe ngcembe iminyaka emibini okanye emine ngaphambi kokuqhushumba. Oku kukhula kwakungeyonto ibaluleke kakhulu, ngaphakathi kwesidanga, nangona kunjalo, incopho ngqo ngexesha lokuqhushumba.

Eyona nto inokwenzeka, oku kungenxa yokuphakanyiswa kwe-magma eshushu kufutshane nomphezulu, kunye neegesi ezishushu. Ukongeza, amanzi asuswe kwiindawo ezingaphezulu komhlaba aququzelela ukubuya kobushushu, ukuphucula umqondiso.

Umthombo: Inzululwazi yezeSwaziya

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