FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2011027309> ?p ?o ?g. }

• W2011027309 endingPage "30084" @default.
• W2011027309 startingPage "30067" @default.
• W2011027309 abstract "Partial pressures of dissolved and atmospheric nitrous oxide, N 2 O, and methane, CH 4 , were measured during the latter stages of the southwest (SW) monsoon and subsequent intermonsoon transition of 1994 in the Gulf of Oman and the northern and central Arabian Sea, during Discovery cruises D210 and D212 of the United Kingdom Joint Global Ocean Flux Study of the northwestern Indian Ocean (NWIO). Mean observed atmospheric mixing ratios, 310±3 ppbv N 2 O, 1706±17 ppbv CH 4 (SW monsoon), and 311±3 ppbv N 2 O, 1784±20 ppbv CH 4 (intermonsoon), were analytically indistinguishable from contemporary global baseline data. Mean surface mixed layer saturations were spatially and temporally heterogeneous. Largest variation was observed for N 2 O in an upwelling region adjacent to the Oman coast; mean N 2 O saturations were 140±40% (SW monsoon) and 119±17% (intermonsoon), with corresponding CH 4 saturations of 170±55% and 179±15%. These apparent differences were largely a consequence of less detailed station coverage during D212, reflecting large variability on a relatively small spatial‐scale rather than true seasonal variation; for individual stations in the coastal upwelling, temporal changes in mean mixed layer saturations were not significant. This suggests that within this region the processes of gas exchange, net production, and supply/removal by advection and vertical mixing were more or less in balance during the period studied. Open ocean saturations were lower and less variable: 106±7% N 2 O, 130±5% CH 4 (SW monsoon) and 104±6% N 2 O, 115±2% CH 4 (intermonsoon). Large supersaturation maxima for N 2 O (saturations ∼400–800%) and CH 4 (saturations ∼200–400%) just below the base of the mixed layer were ubiquitous and followed a trend of progressive deepening toward the south. All deep N 2 O profiles were characterized by a second, more vertically extensive maximum (saturations ∼400–600%) between 500 and 1000 m. For these, plots of ΔN 2 O versus AOU were consistent with their formation by coupled nitrification‐denitrification, with denitrification becoming progressively more important with distance toward the core of the oxygen depleted zone. Sea‐to‐air fluxes for a 6‐month period represented by the study were determined from measured air‐sea partial pressure differences and gas transfer velocities derived from in situ wind speeds. Estimated semiannual emissions, ∼0.41–0.75 × 10 12 g N 2 O, ∼0.1–0.18 × 10 12 g CH 4 , were within most previously reported ranges for the NWIO. The data indicate that seasonal changes in wind speed rather than seasonal changes in air‐sea partial pressure differences due to monsoon‐driven mixing and upwelling are the dominant control on air‐sea gas exchange in the NWIO." @default.
• W2011027309 created "2016-06-24" @default.
• W2011027309 creator A5005752229 @default.
• W2011027309 creator A5006332780 @default.
• W2011027309 creator A5073811999 @default.
• W2011027309 date "1999-12-15" @default.
• W2011027309 modified "2023-10-14" @default.
• W2011027309 title "Nitrous oxide and methane during the 1994 SW monsoon in the Arabian Sea/northwestern Indian Ocean" @default.
• W2011027309 cites W1513196349 @default.
• W2011027309 cites W1658815594 @default.
• W2011027309 cites W1963851862 @default.
• W2011027309 cites W1964810104 @default.
• W2011027309 cites W1966503606 @default.
• W2011027309 cites W1970476342 @default.
• W2011027309 cites W1976365055 @default.
• W2011027309 cites W1976438910 @default.
• W2011027309 cites W1978457402 @default.
• W2011027309 cites W1981574408 @default.
• W2011027309 cites W1984165444 @default.
• W2011027309 cites W1985746264 @default.
• W2011027309 cites W1986390622 @default.
• W2011027309 cites W1989270058 @default.
• W2011027309 cites W1991560340 @default.
• W2011027309 cites W1994806182 @default.
• W2011027309 cites W1995505320 @default.
• W2011027309 cites W1999296078 @default.
• W2011027309 cites W1999575495 @default.
• W2011027309 cites W2003653419 @default.
• W2011027309 cites W2005204485 @default.
• W2011027309 cites W2008009037 @default.
• W2011027309 cites W2009415747 @default.
• W2011027309 cites W2010796731 @default.
• W2011027309 cites W2012118586 @default.
• W2011027309 cites W2016842125 @default.
• W2011027309 cites W2017389604 @default.
• W2011027309 cites W2020395836 @default.
• W2011027309 cites W2021863113 @default.
• W2011027309 cites W2024866771 @default.
• W2011027309 cites W2025005627 @default.
• W2011027309 cites W2025021643 @default.
• W2011027309 cites W2034010438 @default.
• W2011027309 cites W2034773180 @default.
• W2011027309 cites W2037804870 @default.
• W2011027309 cites W2038239334 @default.
• W2011027309 cites W2039743606 @default.
• W2011027309 cites W2047367154 @default.
• W2011027309 cites W2050009747 @default.
• W2011027309 cites W2050238418 @default.
• W2011027309 cites W2051425632 @default.
• W2011027309 cites W2055871082 @default.
• W2011027309 cites W2056107340 @default.
• W2011027309 cites W2058205259 @default.
• W2011027309 cites W2061697548 @default.
• W2011027309 cites W2062093154 @default.
• W2011027309 cites W2063948271 @default.
• W2011027309 cites W2067841165 @default.
• W2011027309 cites W2070161393 @default.
• W2011027309 cites W2073953892 @default.
• W2011027309 cites W2076901722 @default.
• W2011027309 cites W2080648605 @default.
• W2011027309 cites W2081569456 @default.
• W2011027309 cites W2086713933 @default.
• W2011027309 cites W2087927236 @default.
• W2011027309 cites W2093463708 @default.
• W2011027309 cites W2094300388 @default.
• W2011027309 cites W2094841197 @default.
• W2011027309 cites W2098175163 @default.
• W2011027309 cites W2120078519 @default.
• W2011027309 cites W2127865711 @default.
• W2011027309 cites W2131297790 @default.
• W2011027309 cites W2139127544 @default.
• W2011027309 cites W2140361156 @default.
• W2011027309 cites W2151896453 @default.
• W2011027309 cites W2154433734 @default.
• W2011027309 cites W2276077426 @default.
• W2011027309 cites W4236468637 @default.
• W2011027309 doi "https://doi.org/10.1029/1999jc900232" @default.
• W2011027309 hasPublicationYear "1999" @default.
• W2011027309 type Work @default.
• W2011027309 sameAs 2011027309 @default.
• W2011027309 citedByCount "47" @default.
• W2011027309 countsByYear W20110273092012 @default.
• W2011027309 countsByYear W20110273092013 @default.
• W2011027309 countsByYear W20110273092014 @default.
• W2011027309 countsByYear W20110273092015 @default.
• W2011027309 countsByYear W20110273092016 @default.
• W2011027309 countsByYear W20110273092017 @default.
• W2011027309 countsByYear W20110273092018 @default.
• W2011027309 countsByYear W20110273092020 @default.
• W2011027309 crossrefType "journal-article" @default.
• W2011027309 hasAuthorship W2011027309A5005752229 @default.
• W2011027309 hasAuthorship W2011027309A5006332780 @default.
• W2011027309 hasAuthorship W2011027309A5073811999 @default.
• W2011027309 hasBestOaLocation W20110273091 @default.
• W2011027309 hasConcept C105795698 @default.
• W2011027309 hasConcept C111368507 @default.
• W2011027309 hasConcept C121332964 @default.
• W2011027309 hasConcept C122120755 @default.

• next