Matches in SemOpenAlex for { <https://semopenalex.org/work/W2913693564> ?p ?o ?g. }
- W2913693564 endingPage "57" @default.
- W2913693564 startingPage "46" @default.
- W2913693564 abstract "Water resources in the northwestern Himalayas are influenced by the circulation of two dominant weather systems: westerlies and southwest monsoons. The effect of climate change has significantly influenced the overall behaviour of these precipitation bearing climate systems and therefore, the meteorology of the region. To investigate the source, transportation, admixture of vapor sources and post-precipitation modification of stable water isotopic composition (δ18O and δD) of precipitation in the high altitude Himalayan cold desert of Ladakh, upper Indus river basin (IRB) an observational network was established. Monthly composite (n = 110) and event wise precipitation samples (n = 32) were collected during the year 2015–16 for stable water isotopes (δ18O and δD). The stable water isotopic values of the precipitation samples were lower at higher altitude and in January. The monthly δ18O (and δD) of precipitation showed a negative correlation with altitude (R2 = 0.93, p = .001) and temperature (R2 = 0.71 p = .007). However, it was perceived that the stable water isotopic value of precipitation abruptly drops at all the precipitation sites in August, without considerable variation in the ambient temperature and precipitation amount signifying the alteration in moisture source. The NCEP/NCAR reanalysis and back trajectory modeling also corroborates and suggests the modification in the moisture source and reversal of wind pattern during this period. The less d-excess and lower slope (7.4) of local meteoric waterline than the global, regional and local meteoric water lines of western Himalayan, central Himalayas and Kashmir Himalayas indicate the secondary evaporation of falling raindrops below the cloud base. Lagrangian moisture diagnostic was used to recognize the sources, which endorsed the quantitative distinction of different evaporative moisture sources." @default.
- W2913693564 created "2019-02-21" @default.
- W2913693564 creator A5018282820 @default.
- W2913693564 creator A5028965178 @default.
- W2913693564 creator A5045955515 @default.
- W2913693564 creator A5066905294 @default.
- W2913693564 date "2019-06-01" @default.
- W2913693564 modified "2023-10-18" @default.
- W2913693564 title "Stable isotope (δ18O and δD) dynamics of precipitation in a high altitude Himalayan cold desert and its surroundings in Indus river basin, Ladakh" @default.
- W2913693564 cites W1563109307 @default.
- W2913693564 cites W1567962906 @default.
- W2913693564 cites W1950597137 @default.
- W2913693564 cites W1969013333 @default.
- W2913693564 cites W1972017077 @default.
- W2913693564 cites W1979245391 @default.
- W2913693564 cites W1983120929 @default.
- W2913693564 cites W1993338682 @default.
- W2913693564 cites W1993594785 @default.
- W2913693564 cites W1994712116 @default.
- W2913693564 cites W1995988647 @default.
- W2913693564 cites W1999202242 @default.
- W2913693564 cites W2001691937 @default.
- W2913693564 cites W2005528313 @default.
- W2913693564 cites W2012407814 @default.
- W2913693564 cites W2016015255 @default.
- W2913693564 cites W2022833874 @default.
- W2913693564 cites W2029962400 @default.
- W2913693564 cites W2033265152 @default.
- W2913693564 cites W2038546762 @default.
- W2913693564 cites W2039045689 @default.
- W2913693564 cites W2039248536 @default.
- W2913693564 cites W2039785873 @default.
- W2913693564 cites W2039924507 @default.
- W2913693564 cites W2048951374 @default.
- W2913693564 cites W2051934833 @default.
- W2913693564 cites W2054012263 @default.
- W2913693564 cites W2056191382 @default.
- W2913693564 cites W2059615339 @default.
- W2913693564 cites W2064151117 @default.
- W2913693564 cites W2064578721 @default.
- W2913693564 cites W2070263886 @default.
- W2913693564 cites W2076976404 @default.
- W2913693564 cites W2082145563 @default.
- W2913693564 cites W2086316715 @default.
- W2913693564 cites W2089495686 @default.
- W2913693564 cites W2093977941 @default.
- W2913693564 cites W2094780110 @default.
- W2913693564 cites W2095942571 @default.
- W2913693564 cites W2103659921 @default.
- W2913693564 cites W2106867767 @default.
- W2913693564 cites W2110198356 @default.
- W2913693564 cites W2112882251 @default.
- W2913693564 cites W2117267906 @default.
- W2913693564 cites W2117287198 @default.
- W2913693564 cites W2121748480 @default.
- W2913693564 cites W2123060661 @default.
- W2913693564 cites W2129965289 @default.
- W2913693564 cites W2135843060 @default.
- W2913693564 cites W2143373999 @default.
- W2913693564 cites W2146749632 @default.
- W2913693564 cites W2148247314 @default.
- W2913693564 cites W2152609356 @default.
- W2913693564 cites W2164977060 @default.
- W2913693564 cites W2171531906 @default.
- W2913693564 cites W2173251738 @default.
- W2913693564 cites W2189398288 @default.
- W2913693564 cites W2254181589 @default.
- W2913693564 cites W2262383904 @default.
- W2913693564 cites W2279513898 @default.
- W2913693564 cites W2342303920 @default.
- W2913693564 cites W2359132273 @default.
- W2913693564 cites W2417619172 @default.
- W2913693564 cites W2529289890 @default.
- W2913693564 cites W2559523267 @default.
- W2913693564 cites W2577310580 @default.
- W2913693564 cites W2591425496 @default.
- W2913693564 cites W2741303728 @default.
- W2913693564 cites W2752136489 @default.
- W2913693564 cites W2757262932 @default.
- W2913693564 cites W2771000158 @default.
- W2913693564 cites W2793982960 @default.
- W2913693564 cites W2824580773 @default.
- W2913693564 cites W2885378967 @default.
- W2913693564 cites W2891393133 @default.
- W2913693564 cites W4231420001 @default.
- W2913693564 cites W4234326725 @default.
- W2913693564 cites W4245111886 @default.
- W2913693564 cites W4256468369 @default.
- W2913693564 doi "https://doi.org/10.1016/j.atmosres.2019.01.025" @default.
- W2913693564 hasPublicationYear "2019" @default.
- W2913693564 type Work @default.
- W2913693564 sameAs 2913693564 @default.
- W2913693564 citedByCount "59" @default.
- W2913693564 countsByYear W29136935642019 @default.
- W2913693564 countsByYear W29136935642020 @default.
- W2913693564 countsByYear W29136935642021 @default.
- W2913693564 countsByYear W29136935642022 @default.
- W2913693564 countsByYear W29136935642023 @default.