2016, Issue 3, Volume 8

STUDY OF SPATIO-TEMPORAL ANALYSIS OF ANNUAL RAINFALL VARIABILITY IN UTTAR PRADESH

Avadhesh Kumar Koshal* and Prafull Kumar

ICAR-  P.D.F.S.R. College of Agriculture Modipuram, Meerut (U.P.) S.V.P.U.A. &T.,

Meerut (U.P.)

Email: akkoshal@hotmail.com

Received-10.03.2016, Revised-21.03.2016

Abstract: Uttar Pradesh is Humid subtropical and semi arid climatic region situated between 23° 52′ N and 31° 28′ N latitudes and 77° 3′ and 84° 39’E longitudes. The state is divided into 18 divisions and 71 districts. The statistical analysis of annual rainfall data of  past to present 100 years (1915-2014) ranged from 532.7mm  in year in 1991 to 1313.1 mm in year 2013 with an average annual rainfall of the area is 929.6 mm. The  average rainfall  with  2013 showing the highest positive  rainfall anomaly (2.26)  while the other years show rainfall below normal with 1991 Showing the lowest negative rainfall deviation (-2.34). The calculated value of standard deviation reveals that deviation of rainfall is of 169.7 mm. in a century. The trend analysis in XLSTAT 2014.6.02 ver. observed trend of rainfall, the R2 value 0.018 means that only 1.8 percent variation is observed in hundred years. The coefficient of skewness has been computed as -0.06 for annual rainfall indicates a negative trend or going to decline pattern. The maximum  standard deviation value and CV(%)  is observed  210 & 23% in year 1935-44  and minimum standard deviation and CV(%)  is observed  80.7 & 10% in year 1995-04. The overall decadal dataset observed decadal maximum rainfall 1328.9 in year 1955-64 whereas minimum rainfall 493.9mm in year 2005-14 observed. In future, expected annual rainfall may be less in year 2025 observed 881.9mm in the state. In the year 2021; expected rainfall may be 893mm.  The geostatistical analysis is the ARCGIS 10.3.1 extension used for interpolation and kriging. The prediction map of dataset year 1995-2004 was highest rainfall in east side of some place of Uttar Pradesh. The western part of Uttar Pradesh covered less rainfall the other side cover area. The central part of state decadal map covered maximum area in year 1966-74.  The objective of this study is to analyze the recent and future trend of annual rainfall pattern.

Keywords: Anomaly, GIS, Geostatistical method, Kriging & Monsoon

REFERENCES

Adger, W.N.,  Huq, S.,  Brown, K.,  Conway, D. & Hulme, M. (2003). Adaptation to climate change in the developing world, Progress Dev. Stud., 3: 179-195.

Alam, M. M., Toriman, M.  E. bin, Siwar,C. & Talib,B. (2011). Rainfall variation and changing  pattern of agricultural cycle.  American Journal of Environmental Sciences 7 (1): 82-89.

Attri, S.D. and Tyagi, A. (2010). Climate profile of India. India Meteorological Department, Ministry of Earth Sciences, New Delhi: Met Monograph No. Environment Meteorology- 01/2010.

Ayoade, J.O. (1973). Annual rainfall trends and periodicities in Nigeria, Nigerian Geog. J., 16(2):167-176.

Cheng, J., Shi, Z., &  Zhu, Y. (2007). Assessment and mapping of environmental quality in agricultural soils of Zhejiang Province. Journal of Environmental Sciences, 191: 50–54.

Cobanovic, K. (2002). Role of statistics in the education of agricultureal science students . ICOTS6.  1-4.     http://iase-web.org/documents/papers/icots6/4i2_coba.pdf

Dingman, S.L., Seely-Reynolds, D.M. and Reynolds, R.C. (1988). Application of kriging to estimate mean annual precipitation in a region of orographic influence. Water Resour. Bull. 24(2):329-339.

http://www.esri.com/software/arcgis/extensions/geostatistical

India  State of Forest Report (2015). Forest survey of India, Ministry of Environment  & Forests, Govt. of India, Pp. 1-300.

http://fsi.nic.in/isfr-2015/isfr-2015-forest-and-tree-resources-in-states-and-union-territories.pdf

Jang, M., Choi, J., and Lee, J. (2007). A spatial reasoning approach to estimating paddy rice water demand in Hwanghaenam-do, North Korea. Agricultural Water Management, 893:185–198.

Goswami, B.N., Venugopal, V., Sengupa, D., Madhusoodanan,  M.S. & Xavier,  P.K. (2006). Increasing trend of extreme rain events over India in a warming environment, Science. 314:1442-1445.

Guha, G.S. & D.N. Basu (1996). Agroclimtic regional planning in India (Vol.1: concept & applicatons). Pp. 1-235

Haberlandt, U. (2007). Geostatistical interpolation of hourly precipitation from rain gauges and radar for a large-scale extreme rainfall event. Journal of Hydrology, 332: 144–157.

Hutchinson, P. (1985). Rainfall analysis of the Sahelian drought in the Gambia, J. Climatology. 5: 665-672.

Mesnard, L. de (2013). Pollution models and inverse distance weighting: Some critical remarks. Computers & Geosciences. 52: 459-469.

Obot, N.I., Emberga,  T.T. & Ishola, K.S. (2011). 22 years characterized trends of rainfall in Abeokuta, Nigeria, Research Journal of Applied Sciences. 6(4) : 264-271.

http://www.gktoday.in/major-crops-of-india/

Rainfall data: IMD New Delhi, India water Portal & NASA/POWER Agrometeorology webs: India Water Portal (1901-2002 & 2004-2010):                                                

http://www.indiawaterportal.org

IMD (Indian Meteorology Department, New Delhi, (2007 to2013):

www.imd.gov.in

NASA/POWER Agroclimatology Daily Averaged Data (2003 & 2014):

http://power.larc.nasa.gov/common/AgroclimatologyMethodology/Agro1d0_Methodology_Content.html &  http://power.larc.nasa.gov

Rimi, R. H.,  Rahman, S.H.,  Karmakar, S., Hussain. Sk. G. (   ). Trend Analysis of climate change and investigation on Its probable impacts on rice production at Satkhira, Bangladesh. Pakistan Journal of Meteorology. 6 (11).