+ All Categories
Home > Documents > Drought mapping in Poland using SPI

Drought mapping in Poland using SPI

Date post: 11-Feb-2022
Category:
Upload: others
View: 6 times
Download: 0 times
Share this document with a friend
1
Leszek LABEDZKI, Bogdan BAK** ) , Ewa KANECKA-GESZKE, Karolina SMARZYNSKA, Tymoteusz BOLEWSKI Institute of Technology and Life Sciences, Kujawsko-Pomorski Research Centre :: Glinki 60, 85-174 Bydgoszcz, Poland :: [email protected] Since 2012 Institute of Technology and Life Sciences (Poland) has developed the system which provides current and forecasted information on the status and impact of water shortages and surpluses in selected, representative agricultural ecosystems in 13 rural regions of Poland. Most of these selected regions have unfavorable hydro-meteorological conditions for agricultural. This activity is carried out using a nationwide system of automatic meteorological stations. ASSESMENT OF PRECIPITATION CONDITIONS IN POLAND IN JUNE 2013 USING SPI Indicators important for agriculture: soil moisture index SMI, agricultural drought index CDI, potential reduction of crop yield, are calculated using other agro-meteorological factors (air temperature, wind speed, vapor pressure, sunshine duration or radiation, evapotranspiration). The present results of monitoring and forecasts of all indices in the form of maps and tables are shown on-line at the site: www.agrometeo.itep.edu.pl . The standardized precipitation index SPI is used for monitoring and forecasting precipitation deficits and surpluses. The SPI is calculated for each month at the 1-, 2-, 3-, 6-, 12-, 24-, 36- and 48- month time scale. SPI1, SPI2 - shorter time scale indexes describe drought events affecting agriculture (soil moisture depleting, crop yield reduction), SPI3, SPI6 is used for seasonal drought identification SPI12, SPI24, SPI48 - for a long-term drought identification, suitable for water resources hazard (reservoirs storage, stream flows, groundwater levels) Extreme drought Severe drought Moderate drought Mild drought Normal Wet Moderately wet Very wet Extremely wet meteorological stations FORECAST OF PRECIPITATION CONDITIONS USING SPI DESCRIPTION OF MONITORING SYSTEM STANDARDIZED PRECIPITATION INDEX SPI agrometeo.itep.edu.pl. * Project is financed by Polish Ministry of Agriculture and Rural Development Programme: Monitoring, Predicting of Progress and Risk of Water Deficit and Surplus in the Rural Areas, 2011 2015. ** Bogdan Bak, PhD poster presenter, meteorologist and agrometeorologist superviser collecting meteorological data and preparing meteorological forecast on the basis of MeteoGroup Poland and WetterOnline models REFERENCES McKee T.B., Doesken N.J., Kleist J. The relationship of drought frequency and duration to time scales. Proc. 8th Conf. Applied Climatology, 17-22 January 1993. Anaheim, California, 1993, pp. 179-184. McKee T.B., Doesken N.J., Kleist J. Drought monitoring with multiple time scales. Preprints 9th Conf. Applied Climatology, 15-20 January 1995. Dallas, Texas, 1995 pp. 233-236. Hunt E.D., Hubbard K.D., Wilhite D.A., Arkebauer T.M., Dutcher A.L. The development and evaluation of a soil moisture index. International Journal of Climatology, 2008. Published online in Wiley InterScience (www.interscience.wiley.com) DOI: 10.1002/joc.1749. Labedzki L., Bak B. 2013. Monitoring and forecasting the course and impact of water deficit in rural areas. Ekologia Terenów Wiejskich. Nr 2/I pp. 65-76. Weather forecasts, necessary to develop predictions of water shortages or surpluses in the next 10 and 20 days, come from the meteorological service of MeteoGroup Poland and WetterOnline. Selected Regions in Poland Soil moisture conditions in late potato cultivation based on the soil moisture index (SMI) in the period 21 - 30 June 2013 and 10 and 20 day forecast. a) - light soil, b) moderate soil
Transcript
Page 1: Drought mapping in Poland using SPI

Leszek LABEDZKI, Bogdan BAK**), Ewa KANECKA-GESZKE, Karolina SMARZYNSKA, Tymoteusz BOLEWSKI

Institute of Technology and Life Sciences, Kujawsko-Pomorski Research Centre :: Glinki 60, 85-174 Bydgoszcz, Poland :: [email protected]

Since 2012 Institute of Technology and Life Sciences (Poland) has

developed the system which provides current and forecasted

information on the status and impact of water shortages and

surpluses in selected, representative agricultural ecosystems in 13

rural regions of Poland. Most of these selected regions have

unfavorable hydro-meteorological conditions for agricultural. This

activity is carried out using a nationwide system of automatic

meteorological stations.

ASSESMENT OF PRECIPITATION CONDITIONS

IN POLAND IN JUNE 2013 USING SPI

Indicators important for agriculture: soil moisture index SMI,

agricultural drought index CDI, potential reduction of crop yield, are

calculated using other agro-meteorological factors (air

temperature, wind speed, vapor pressure, sunshine duration or

radiation, evapotranspiration).

The present results of monitoring and forecasts of all indices in the

form of maps and tables are shown on-line at the site:

www.agrometeo.itep.edu.pl.

The standardized precipitation index SPI is used for monitoring and

forecasting precipitation deficits and surpluses. The SPI is

calculated for each month at the 1-, 2-, 3-, 6-, 12-, 24-, 36- and 48-

month time scale.

SPI–1, SPI–2 - shorter time scale indexes describe drought

events affecting agriculture (soil moisture depleting, crop yield

reduction),

SPI–3, SPI–6 is used for seasonal drought identification

SPI–12, SPI–24, SPI–48 - for a long-term drought identification,

suitable for water resources hazard (reservoirs storage, stream

flows, groundwater levels)

Extreme drought

Severe drought

Moderate drought

Mild drought

Normal

Wet

Moderately wet

Very wet

Extremely wet

● meteorological stations

FORECAST OF PRECIPITATION CONDITIONS

USING SPI

DESCRIPTION OF MONITORING SYSTEM

STANDARDIZED PRECIPITATION INDEX SPI

agrometeo.itep.edu.pl.

* Project is financed by Polish Ministry of Agriculture and Rural Development Programme:

Monitoring, Predicting of Progress and Risk of Water Deficit and Surplus in the Rural Areas, 2011

– 2015.

** Bogdan Bak, PhD – poster presenter, meteorologist and agrometeorologist superviser

collecting meteorological data and preparing meteorological forecast on the basis of MeteoGroup

Poland and WetterOnline models

REFERENCES

McKee T.B., Doesken N.J., Kleist J. The relationship of drought frequency and duration to time

scales. Proc. 8th Conf. Applied Climatology, 17-22 January 1993. Anaheim, California, 1993, pp.

179-184.

McKee T.B., Doesken N.J., Kleist J. Drought monitoring with multiple time scales. Preprints 9th

Conf. Applied Climatology, 15-20 January 1995. Dallas, Texas, 1995 pp. 233-236.

Hunt E.D., Hubbard K.D., Wilhite D.A., Arkebauer T.M., Dutcher A.L. The development and

evaluation of a soil moisture index. International Journal of Climatology, 2008. Published online in

Wiley InterScience (www.interscience.wiley.com) DOI: 10.1002/joc.1749.

Labedzki L., Bak B. 2013. Monitoring and forecasting the course and impact of water deficit in

rural areas. Ekologia Terenów Wiejskich. Nr 2/I pp. 65-76.

Weather forecasts, necessary to develop predictions of water

shortages or surpluses in the next 10 and 20 days, come from the

meteorological service of MeteoGroup Poland and WetterOnline.

Selected Regions in Poland

Soil moisture conditions in late potato cultivation based on the soil moisture index

(SMI) in the period 21 - 30 June 2013 and 10 and 20 day forecast.

a) - light soil, b) – moderate soil

Recommended