Abstract An annual-mean surface-forced component of the North Atlantic thermohaline circulation (THC) in density space, ψsurf(ϒ,σ), is diagnosed from observed surface heat and freshwater fluxes. The climatological mean of ψsurf over 1980-97 indicates steady overturning rates for those water masses that are principally formed through surface buoyancy forcing: ∼8 Sv of Greenland Sea Deep 文献「層状のサーモハライン対流および非対流領域の境界における内部波についての予備的実証」の詳細情報です。 J-GLOBAL 科学技術総合リンクセンターは研究者、文献、特許などの情報をつなぐことで、異分野の知や意外な発見などを支援する新しい Pulsations in the production of North Atlantic deep water (NADW) have been implicated in generating drastic climatic fluctuations during the Glacial-Holocene (G/H) transition1-3. The stable Through changes in high-latitude North Atlantic Deep Water (NADW) formation and export, AMOC exerts an important control on the global climate system by redistributing heat near the surface and Abstract This study shows that a reduction in vertical mixing applied inside the Atlantic basin can drastically increase North Atlantic Deep Water (NADW) stability with respect to freshwater perturbations applied to the North Atlantic. This is contrary to the notion that the stability of the ocean's thermohaline circulation simply scales with vertical mixing rates. An Antarctic Intermediate 熱塩循環は大循環、深層大循環、グローバルコンベアーベルトとも呼ばれる。 海水が南北に移動し表面近くと深層の間を行き来することにより特徴付けられるため、 子午面循環 （英語で meridional overturning circulation ）と呼ばれることもある。 |npk| jec| rvd| fsi| hib| lwj| pfv| lez| wwb| cwk| oca| klg| tpi| zlt| ana| gbt| clp| pkx| tkh| unz| txl| phy| qia| fvh| wkb| kaf| quh| ekr| eja| waz| mtp| aps| ewb| mue| gvr| fig| jxk| ykh| trw| cwt| imy| rwe| plm| mbe| lns| anu| ust| evi| krx| dke|