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This work is licensed under a Creative Commons Attribution 4.0 International License.
Historically Heavy Rainfalls in Singapore on 19 November 2009 and 17 July 2010
Corresponding Author(s) : Hidemitsu Katsura
Asian Journal of Chemistry,
Vol. 25 No. 4 (2013): Vol 25 Issue 4
Abstract
On 19 November 2009 and 17 July 2010, historically heavy rainfalls occurred in Singapore. Aerosol samples (PM 4.5) were collected with a sampling pump at a flow rate of 5 L per min from 16 to 22 November 2009, from 08 to 20 February 2010 and from 16 to 28 July 2010. Rainwater samples were collected every 5 mL of rainfall using an Horiba Raingoround sampler from 17 to 21 November 2009, from 10 to 18 February 2010 and from 16 to 28 July 2010 on a rooftop at the National University of Singapore in Singapore. These samples were analyzed by ion chromatography for anions and by gas chromatography-mass spectrometry for nitrogen and oxygen stable isotope ratios. During periods of historically heavy rainfall, the d18O/16O ratios in nitric-oxide substances in aerosols tend to decrease tremendously. The 14N atoms in nitrogen oxide ions in rain drops are converted to 14C through neutron-activated nuclear chemical reactions at higher altitudes. Consequently, d15N/14N ratios increase with the production altitudes of rain drops. Therefore, figures displaying the d15N/14N ratios of nitrogen oxide ions in different separated rainfall fractions have a characteristic form. This implies that there is some relationship between the chemical characterization of aerosols and the chemical characterization of rainfall.
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References
M. Samuel, J. Savarino, F.M. Markus, N. Yan, S. Bekki, J.W. Bottenheim and M.F. Jean, Science, 322, 730 (2008).
K. Baechmann, P. Ebert, I. Haag, T. Prokop and K. Steigerwald, Atmos. Environ., 30, 1019 (1996).
M.A. Benson, Factors Influencing the Occurrence of Floods in a Humid Region of Diverse Terrain, US Geological Survey Water Supply Paper (1962).
G. Blöschl and M. Sivapalan, Scale Issues in Hydrological Modeling: A Review, Scale Issues in Hydrological Modeling. Wiley, 9-48 (1995).
T. Dalrymple, Flood Frequency Analyses, Manual of Hydrology: Part 3, Flood Flow Techniques, USGS Water Supply Paper 1543-A (1960).
D. Ehhalt, M. Prather, F. Dentener, R. Derwent, E. Dlugokencky, E. Holland, I. Isaksen, J. Katima, V. Kirchhoff, P. Matson, P. Midgley and M. Wang, Atmospheric Chemistry and Greenhouse Gases, in: Climate Change (2001), The Scientific Basis Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change, in eds.: J.T. Houghton, Y. Ding, D.J. Griggs, M. Noguer, P.J. van der Linden, K. Dai, K. Maskell and C.A. Johnson, Cambridge University Press, New York, USA (2001).
Y. Fang, K. Koba, X.M. Wang, D.Z. Wen, J. Li, Y. Takebayashi, X.Y. Liu and M. Yoh, Atmos. Chem. Phys., 11, 1313 (2011).
S. Kundu, K. Kawamura, T.W. Andreae, A. Hoffer and M.O. Andreae, J. Aerosol Sci., 41, 118 (2010).
J. Savarino, K. Kaiser, S. Morin, D.M. Sigman and M.H. Thiemens, Atmos. Chem. Phys., 7, 1925 (2008).
W.P. Winn, C.B. Moore, C.R. Holmeset and L.G. Byerley III, J. Geophys. Res., 83, 3079 (1978).
W.C. Lim, There was just too much rain, The Strats Times 20 NOV 2009 A1, A8 (2009).
M. Hetty, Heavy Rain Causes Flash Floods in Hotspots, Leaves Trail of Damage and Disruption (Posted: 17 July 2010 1318 SST) (Accessed: 19 July 2011) http://www.channelnewsasia.com/stories/singaporelocalnew/view/1069917/1/.html
K.L. Casciotti, D.M. Sigman, M. Galanter Hastings, J.K. Böhlke and A. Hilkert, Anal. Chem., 74, 4905 (2002).
Y. Takebayashi, K. Koba, Y. Sasaki, Y. Fang and M. Yoh, Rapid Commun. Mass Spectrom., 24, 1001 (2010).
P. Richet, Y. Bottinga and M. Javoy, Ann. Rev. Earth Planet. Sci., 5, 65 (1977).
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N. Feather, Proc. Royal Soc. London, Series A, 136, 830 (1932).
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W. Harkins, Phys. Rev., 44, 529 (1933).
O. Haxel, J.H.D. Jensen and H.E. Suess, Phys. Rev., 75, 1766 (1949).
W.F. Libby, Phys. Rev., 69, 671 (1946).
C.B. Ramsey, Archaeometry, 50, 249 (2008).
E. Rutherford, Proc. Royal Soc. London, Series A, 97, 374 (1920).