W. Palmer, “Meteorological Drought,” Research Paper, US.

Palmer, WC (1965). Meteorological drought. U.S. Research Paper No. 45. US Weather Bureau,Washington, DC.

The risk of drought is subject to a combination of frequency, severity and its spatial extent, and the vulnerability of a population or activity (4)(5)(6)(59)(60)(61) Meteorological factors, soil.

Comparison of Two Drought Indices for Drought Monitoring in Hungary — A Case Study. Authors; Authors and affiliations; S. Szalai; Cs. Szinell; Chapter. 29 Citations; 431 Downloads; Part of the Advances in Natural and Technological Hazards Research book series (NTHR, volume 14) Abstract. This paper presents two indices developed for drought monitoring purposes. In a first step, the need for.

In 1965 Wayne C. Palmer, a scientist in the Office of Climatology, Weather Bureau, US Department of Commerce, Washington, DC, published a research paper entitled “Meteorological drought”. Applications of the analytic procedures set forth in this paper have become widely known as the Palmer Index or the Palmer Drought Severity Index (PDSI). It is a hydrologic or persistent climatological.

Palmer Hydrological Drought Index (PHDI). 1965: Meteorological Drought. Research Paper No. 45. United States Weather Bureau, Washington, DC. Currently used by: Trinidad and Tobago. 11 Comments temesgen fikadie. January 3, 2017 Reply. please send your work on hydrlogical drought analysis based on different drought analysis indce pdf in detail. temesgen fikadie. January 3, 2017 Reply. i am a.

How to Cite. Morid, S., Smakhtin, V. and Moghaddasi, M. (2006), Comparison of seven meteorological indices for drought monitoring in Iran. Int. J. Climatol., 26: 971.

The Palmer drought index, sometimes called the Palmer drought severity index and often abbreviated PDSI, is a measurement of dryness based on recent precipitation and temperature. It was developed by meteorologist Wayne Palmer, who first published his method in the 1965 paper Meteorological Drought for the Office of Climatology of the U.S. Weather Bureau.

Palmer Drought Severity Index: attempts to measure the duration and intensity of the long-term drought-inducing circulation patterns. Long-term drought is cumulative, so the intensity of drought during the current month is dependent on the current weather patterns plus the cumulative patterns of previous months. Since weather patterns can change almost literally overnight from a long-term.

How to Cite. Patel, N. R., Chopra, P. and Dadhwal, V. K. (2007), Analyzing spatial patterns of meteorological drought using standardized precipitation index.

Drought is a natural local or regional phenomenon, its basic cause being the lack of precipitation over a time period. Drought may be studied from the environmental or the water resources point of view ().Environmental droughts can be classified into meteorological drought, hydrological drought and agricultural drought.

Drought is a normal phenomenon of earth’s climate, and is a common feature in the drylands of India. Indian agriculture, which is highly dependent on the monsoon rainfall, is a major victim of drought. Since nearly 70% of the net sown area in the country is rainfed, aberrant behavior of the monsoon such as low and poor rainfall distribution, its delayed onset, or prolonged dry spells during.

Drought Policies and Impacts in Rajasthan, India M. S. Rathore Drought Series. Paper 6. i Working Paper 93 Drought Series Paper No. 6 STATE LEVEL ANALYSIS OF DROUGHT POLICIES AND IMPACTS IN RAJASTHAN, INDIA M. S. Rathore International Water Management Institute. ii The authors: Dr Manohar Singh Rathore is a Senior Fellow at the Institute of Development Studies, Jaipur, Rajasthan, India This.