ࡱ> q`bjbjqPqP 8::gB uuu8vvNJx`x`x`x`x;y;y;yVXXXXXX$9hJ|)R;y;yRR|`x`xRZ `x`xVRV`x>x 0no!u ڙ| 0~@;yN|\~ɀ;y;y;y||4R;y;y;yRRRRdYJbJb PRECIPITATION AND TEMPERATURE INFLUENCES ON MAIZE YIELDS IN EASTERN CROATIA Kova evi V. Abstract Maize is the most widespread crop on arable lands in Croatia. It occupies about 0.4 million hectares or a fourth of arable land areas. In general, under environmental conditions of Eastern Croatia, there is usually a close connection between low maize yields and precipitation shortage combined with high air-temperatures. Two growing seasons (2000 and 2003) were especially unfavorable for maize growing. For example, low yields for 2000 (34% lower in comparison with four previous years) is mainly influenced by water deficit. In 2003 they were in association with drought in June-August (30% lower precipitaion) combined with high air-temperatures - mean 23.3 oC or for 2.8 oC higher than 30-year mean. Water deficit becoming main limiting factor of maize yields in Eastern Croatia under dry farming system. The objective of this study was to examine association between maize yield and weather characteristics. Irrigation is needed for minimizing annually yield variations. Key words: maize, grain yield, precipitation quantities, Eastern Croatia INTRODUCTION Maize is the most widespread crop on arable lands in Croatia. It occupies about 0.4 million hectares (mean 2001-2003 = 406 thousands ha) or a fourth of arable land areas of the country. In the earlier period maize harvested areas were about 0.5 million hectares (20-year mean 1971-1980 = 503300 ha). Maize grain yields in Eastern Croatia are about 30% higher in comparison with mean yields of the country. Besides the degree of soil fertility, precipitation and temperature regimes during a growing season significantly influence maize yields as well. This problem is curetting by climate change (Lang et al., 2006). In general, under environmental conditions of Eastern Croatia, there is usually a close connection between low maize yields and precipitation shortage, especially during the two summer months, July and August (Josipovi et al., 2005; Kova evi and Kau i, 2006; Kova evi et al. 2007; `oatari and Josipovi, 2006). This phenomenon is mainly more influencing factor in the eastern part of the region in comparison with its western part because of prevailing of more aerated soils. These findings are consistent with experiences from the USA Corn Belt (Shaw, 1988). The objective of this study was to examine association between maize yield and weather characteristics (temperature and precipitation regimes). ________________________________________________________________________ Revial paper; Prof. Dr. Vlado Kova evi, scientific adviser, University J. J. Strossmayer in Osijek, Faculty of Agriculture, Trg Svetog Trojstva 3, HR-31000 Osijek, Croatia; e-mail:  HYPERLINK "mailto:vkovacevic@pfos.hr" vkovacevic@pfos.hr MATERIAL AND METHODS Description of the territory and sources of the data The region of Eastern Croatia until 1992 covered 11090 km2 or 19.6% of the state territory and it was divided in 14 municipalities. Since 1992, according new territorial division the Eastern Croatia covers five counties of total area 12452 km2 (or 21.9 % of the state territory) as follows: Vukovar-Syrmium, Brod-Posavina, Osijek-Barannya, Pozega-Slavonia and Virovitica-Podravina County. The data of State Bureau for Statistics were used as source of grain yields data. State Hydrometeorological Institute was source of meteorological data (precipitation and mean air-temperatures). War escalation in Croatia from 1991 to 1995 was reason that maize yields data were uncompleted. Also, in this period field crop yields were low, mainly as affected by war-induced factors. For this reason, only data for the period 1996-2005 were shown (with exception of data for 2004 because Statistical Yearbook has not contains data of yields and arable crops harvested areas). Also, the internal data of the former state farms (SF)  Jasinje Slav. Brod, SF  akovo and SF  Kutjevo were used (Tables 3 and 4). Climate, relief, geomorphologic, geologic and pedological features of Eastern Croatia The Pannonian part of Croatia has temperate continental climate with four clearly differentiated seasons. All climatic elements manifest certain changes on going from the east to the west. The eastern part (the region eastern Croatia) is characterized by dry and torrid summers and harsh winters, in contrast to the western part with considerably higher precipitation and smaller temperature amplitudes. For example, the average monthly precipitation in Osijek and Zagreb amounts to 660 and 854 mm, respectively. The mean annual temperature decreases in the same direction from 10.9 (Osijek) to 9.9 oC (Varazdin). Eastern Croatia occupies the eastern part of the Pannonian Croatia. With regard of the field crops growing, especially maize and wheat, this region is very important. Geomorphologically, Pannonian Croatia constitutes a spacious plain with three geomorphologic and geological-lithological units as follows: the Holocene terrace, the Pleistocene terrace and the Midslavonian Mountains (Janekovi et al. 1971; `kori et al. 1985). Their relief, geomorphologic, geologic and pedological characteristics with aspect of arable crops growing were shown in the previous study (Kovacevic et al., 2007). RESULTS AND DISCUSSION In the least four-decade period maize yields in Croatia have increasing trend with high degree of their variation among the years. For example, the lowest annually yield was for 27% lower than maximal annual yield for both decade periods (1971-1990), while in the period 1996-2005 it was for even 44% lower. Maize yields in Eastern Croatia region are higher (27%, 25% and 16%, for the first, second and third tested decade, respectively) compared to the state mean. In the 1996-2005 period, maize harvested area in Croatia decreased about 25% in comparison with 20-year mean of 1971-1990, whereas yields showed mild increasing trend (Table 1). Maize yield for 1996-2005 decade period in VSc was for 11% higher in comparison with mean yield of remaining four counties ( 6.73 and 6.04 t/ha, respectively), mainly as affected by prevailing of more fertile soils in this part of the region (Janekovi, 1971). In general, maize yields were lower in the growing seasons characterizing the lower precipitation and the higher air-temperatures compared to long-term means. Also, under water shortage conditions maize yield differences among the counties are mainly lower (Table 2). In the last decade period (1996-2005) two growing seasons (2000 and 2003) were especially unfavorable for maize growing. For example, low maize yield in the region of Eastern Croatia in 2000 (34% lower in comparison with four previous years) is mainly influenced by water shortage. Low yields of maize for the 2003 growing season were in association with water deficite in June-August period (30% lower in comparison with long-term mean) combined with extremelly high air-temperatures - mean 23.3 oC or for 2.8 oC higher than 30-year mean (Table 2). Drained hydromorphic soils are dominant soil types of the SF Jasinje Slav. Brod. In the past, excess of water was also limiting factor of maize yields in this area, but after draining water deficit (Table 3) and nutritional problems (mainly low levels of plant available phosphorus) became main limiting factors of maize yields (Petosic et al., 2003). Table 1. Maize harvested area and grain yields in Croatia, Eastern Croatia region as well Tabela 1. Po~ete povraine i prinosi zrna kukuruza u Hrvatskoj i u regiji isto ne Hrvatske Maize harvested area (ha) and yields (t/ ha) / Po~ete povrine(ha) i prinosi kukuruza (t/ha)The 1971-1980 periodThe 1981-1990 periodThe 1996-2005 period*Year/God.hat/haYear/God.hat/haYear/God.hat/haRepublic of Croatia / Republika Hrvatska1971 1972 1973 1974 1975506567 489086 516292 480311 5303613.35 3.39 3.56 3.86 4.151981 1982 1983 1984 1985518615 494235 511753 501313 5286604.62 5.03 4.85 5.33 4.851996 1997 1998 1999 2000361000 371000 378000 384000 3883385.22 5.88 5.25 5.56 3.931976 1977 1978 1979 1980503646 501556 465842 487939 4838073.84 4.50 4.04 4.56 4.141986 1987 1988 1989 1990531589 495946 511224 503378 5038765.16 4.44 3.92 4.44 3.872001 2002 2003 2004 2005406000 407000 406515 - 3189315.45 6.14 3.86 - 6.92Mean4965413.94Mean5100594.65Mean3800875.3620062961956.53Eastern Croatia / Isto na Hrvatska1971 1971 1973 1974 1975208892 195942 216172 192182 2216324.06 4.67 4.30 5.16 5.141981 1982 1983 1984 1985214301 201268 209305 206779 2213955.72 6.40 6.40 7.08 6.261996 1997 1998 1999 2000154202 159770 169935 177353 1801826.30 7.01 6.20 6.50 4.311976 1977 1978 1979 1980201462 196650 180862 196632 1896924.76 5.80 5.14 5.87 5.421986 1987 1988 1989 1990217788 197149 209768 208312 2341486.59 5.33 4.78 5.46 4.312001 2002 2003 2004 2005190136 185651 184270 - 1485796.63 7.21 4.49 - 7.29Mean2000125.03Mean212 0215.83Mean1722316.22*with exception of the 1991-1995 (uncompleted data and low yields mainly by war-induced factors) and 2004 (not issued completed Statistical yearbook) period * s izuzetkom perioda 1991-1995 (nekompletni podaci i niski prinosi izazvani uglavnom ratnim prlikama) i 2004 (nekopmletno izdanje Statisti kog godianjaka) Table 2. Grain yields of maize (t/ha) in Eastern Croatia (the 1996-2005 period and weather data for Osijek Tabela 2. Prinosi zrna kukuruza (t/ha) u isto noj Hrvatskoj u periodu 1996-2005 i meteoroloaki podaci za Osijek Year God.Maize yield (t/ ha) Prinos kukuruza (t/ha)Precipitation (mm) and mean air-temp. (oC) in Osijek /Padaline i temp. zrakaThe county (c)* / }upanija*JuneJulyAugustVScOBcVPcBPcPScmmoCmmoCmmoC1996 1997 1998 1999 20007.06 7.29 6.49 7.29 4.726.46 7.35 6.53 6.60 3.965.84 6.83 5.88 5.82 4.306.15 6.37 5.48 5.62 4.305.73 6.76 5.59 5.97 4.6730 86 26 150 1021.1 20.8 21.4 20.3 22.595 91 84 95 6319.9 20.3 22.2 21.9 21.777 41 99 74 520.6 20.5 21.8 21.3 23.72001 2002 20037.37 6.82 5.156.79 7.50 4.325.94 7.67 4.575.77 6.42 3.985.94 6.46 4.53240 36 4418.1 21.1 24.377 59 6121.6 22.3 22.1 7 77 4122.7 20.9 23.62004 data not available /nema podataka7719.24321.59621.020058.386.986.597.167.4311219.517121.523819.3Mean6.736.285.946.035.908120.88421.57621.52006usual yields / uobi ajeni prinosi9120.11523.513319.3Averages / Proseci: 1961-19908819.56521.15820.3* the counties (c): Vukovar-Sirmium (VSc), Osijek-Baranya (OBc), Virovitica-Podravina (VPc), Brod-Posavina (BPc) and Pozega-Slavonia (PSc). *~upanije: Vukovarsko-srijemska, Osje ko-baranjska, Viroviti ko-Podravska, Brodsko-posavska i Po~eko-slavonska. Table 3. Influences of weather conditions on maize yields on the state farm Jasinje and weather data of Slav. Brod Weather Bureau (Petosic et al., 2003) Tabela XX. Uticaj vremenskih prilika na prinose kukuruza na Agrokombinatu  Jasinje i meteoroloaki podaci za Slav. Brod (Petoai i sur., 2003) Grain yields of maize on AK Jasinje Slavonski Brod and weather data Prinosi kukurza na AK  Jasinje i meteoroloaki podaci za Slav. BrodLess favorable years  Nepovoljne godineMore favorable years  Povoljne godineAverage Prosek19871988198619891971-1990 Maize yields (t/ha) on AK Jasinje (in the bracket: harvested area in ha) Prinosi kukuruza (t/ha) na AK  Jasinje (u zagradi: po~eta povraina u ha)5.42 (3173)4.35 (2963)7.72 (3525)7.02 (2781)5.42 (3231)Month MesecPrecipitation (mm) and mean air-temperatures (oC) - Slavonski Brod Padaline (mm) i srednje temp. vazduha (oC) - Slavonski BrodmmoCmmoCmmoCmmoCmmoCJan.- March18419820563129April - Sept.30217.929917.940217.458417.142616.9July + Aug.8621.49722.418920.114920.515820.0 Influences of water and temperature regimes on maize yields in the most remaining SF of the region are similar as for Jasinje (for example, the SF  Vprx    , = > G ƻyePePey@h"h"6CJaJmH sH )h"h"6CJH*PJmHnHtHu&h"h"6CJPJmHnHtHuh"h"6CJh"h"6CJmH sH h"h"6mH sH h30h"56mH sH hjUmH sH hXmH sH hL[hvmH sH h"hv5mH sH h"5mH sH h"hX5mH sH h"h}5mH sH h"h5mH sH r= > $a$gd[_=$a$gdzWB$a$gdzWB$a$gd"$a$gd"$a$gd*$a$gd"G Bxv6r.YstzJ<>ƼƲƼƔƊƊƊƊƊƂzrgXgjhL[h[_=UmH sH hL[h[_=mH sH hjUmH sH hvmH sH h[_=mH sH hcMCJmH sH h|GCJmH sH h_RCJmH sH h<CJmH sH hNdBCJmH sH h}CJmH sH hL[hzWBCJmH sH hL[hvmH sH h"hjU6mH sH h"6mH sH h"h"6mH sH "(abc4=?Kk|ƻ|qj_qTLThQmH sH h9hhQmH sH h9hhl ImH sH  h9hhh9hhAmH sH h9hhN"H* h9hhN"h9hhmH sH h9hhN"H*mH sH h9hhN"mH sH h9hhN"6>*mH sH hYbhvmH sH hL[h[_=mH sH hL[h[_=0JmH sH jhL[h[_=UmH sH #jhL[h[_=UmH sH (2 ####r&*,".$..//%0 $$Ifa$gdi$a$gdY$a$gd9h$a$gdp$a$gd*$a$gd$a$gdN"npx" # 2 3 """@"\""r#t#v######$$@%T%f%m%%廴|qjcj_jcjh|G h$hA h$hph_RhvmH sH  h>hN" h>hL[ h>hu% hL[hu% hL[hL[hu%h>hL[ hN"H*hN" h9hhN"h9hhN">*h9hhL[>*h9hhL[6>*h9hhL[6>*aJmH sH h9hhN"6>*aJmH sH h9hhmH sH "%f&r&*N,n,w,y,,,,,,,,,,,- .".$.&.`.n.......//ϰϰϡ{rl{f{l`V{hh6CJ hYCJ hmXCJ hCJhYhCJhYhYCJ hX@CJh<_hcW+hkI hah: h: hM0PJmHnHsHtHu"hgq hpH*PJmHnHtHuh~;PJmHnHtHuhgq hpPJmHnHtHu hgq hp h$hp#h$hpPJmHnHsHtHu ///////$0d0f0g0k0l0p0q0y0~00000000000000112xmbSShUMhYCJaJmH sH hYh{ mH sH hYh{ mH sH hh6mH sH hmH sH h{ mH sH hYhYmH sH hh6CJaJmH sH hhCJaJmH sH hhYCJaJmH sH hYhYH*mH sH hh6mH sH hYmH sH hmH sH hYhYmH sH  %0&0;0P0f0 $$Ifa$gdgkd$$Ifl7 t0644 laf0g0q0t0y00000000qeeeeeeeee`Ff $$Ifa$gdkdK$$IflF d7   t06    44 la 0000000000001 1111gkd$$Ifl7 t0644 la $$Ifa$gd11"1'1,11161=1D1K1R1Y1^1c1h1m1r1w1|11111111111 $$Ifa$gd111111111111112 22222"2'2,21262=2D2K2Ff $$Ifa$gdK2R2Y2^2c2h2m2r2w2|2222222222222222222Ff $$Ifa$gd22222222222222 3 334 4"4$4V4\4d4j4r4x4444455555"5ɽɽɽծ|m^m^m^m^m^m^m^m^hUMh>CJaJmH sH hUMhoMCJaJmH sH hYh{ mH sH hh6mH sH hmH sH h{ mH sH hYh-}mH sH hUMh-}CJaJmH sH hUMhv+ 6mH sH hUMhY6mH sH hYhYmH sH hUMhYCJaJmH sH hUMhYCJH*aJmH sH $222222222222223 3 3"4 $$Ifa$gd{ FfmFfC $$Ifa$gd"4$4.484B4L4V4d4r444444444 $$Ifa$gdgRPgkdk$$Ifl7 t0644 la44444555*585F5P5Z5d5n5x55555555555566 $$Ifa$gdgRP"5*50585>566+6.6265696<6@6C6G6J66666666666 7 777777 7-7278797=7>7?7G7`7x77778ĻįϧϧĚh_Rh6CJhYCJmH sH hYhYCJmH sH hM0mH sH hrShLu\mH sH h>\mH sH hYhLumH sH hLumH sH hYhoMmH sH hUMh>CJaJmH sH hUMhoMCJaJmH sH 06 66666!6&6+62696@6G6N6S6X6]6b6g6l6q6v6{666666Ff; $$Ifa$gdgRP666666666666666666677 7 7777 7 $$Ifa$gd"8Ffy $$Ifa$gdgRP 7(7-72797>7?778889::::: ;; $$Ifa$gdv $Ifgd0 $$Ifa$gdi$a$gdN$a$gd|gdAgdYFf $$Ifa$gd"88888899"94989h999999999p:r::::::::ƾγΔwh`[QFh<hE&mHsHhE&hE&6\ hN\h8hN\hKhNCJaJmH sH h:h:6h6mH sH h:h:6mH sH h@bmH sH hE&hE&mH sH hhE&mH sH hh0mH sH h:mH sH h0mH sH hh@bmH sH hjUh_Rh6CJmH sH h_Rh6CJh_RhgRP6CJ:::;;; ;n;p;t;;;;;;;;;<< <<<<#<üzumbVmJ>h8hv\mH sH h8hv\mH sH hNh@b\mH sH h8h@bmH sH h8hv\ hE&\h8h{nT\h8h@b\hNhN\ h8hNhE&hE&6hE&h8hvmH sH h8hvH*mH sH  h8hvh<hN\mHsHh<h0mHsHh<hE&6mHsHh<hE&mHsHh<hE&CJaJmHsH;;;;<< <wk_kVV $Ifgdi $$Ifa$gdi $$Ifa$gdikd$$Ifl4F0 0    4 lalf4 <<<<<<<#<QEEEEEE $$Ifa$gdikdk$$Ifl4rz*0 z04 lalf4#<&<)<,</<2<5<6<;<@<E<J<O<T<Y<^<c<h<m<r<w<|<<<< $$Ifa$gdFf $$Ifa$gd+t $$Ifa$gdi#<&<'<,<-<2<3<5<6<O<<D=E=T============> >$>V>X>b>>>>ξβξΣΔΔβ΄tbξZh[NmH sH "hUMhE&6CJ\aJmH sH hUMh/`RCJ\aJmH sH hUMhE&CJ\aJmH sH hUMh.gCJaJmH sH hUMhCY4CJaJmH sH hNh8\mH sH hUMh8CJ\aJmH sH hUMh8CJaJmH sH hNhv\mH sH h8hvH*mH sH h8hvmH sH !<<<<<<<<<<<<<<<<<<<<<<<<<<< $$Ifa$gd[N $$Ifa$gdi<== ===== =#=&=)=+=0=5=:=?=D=E=J=O=T=Y=^= $$Ifa$gdFf# $$Ifa$gdi $$Ifa$gd+t $$Ifa$gd[N^=c=h=m=r=w=|=================== $$Ifa$gd+t $Ifgd8 $$Ifa$gd[N $$Ifa$gdi==========&>,>6><>F>L>V> $$Ifa$gd[N $IfgdE& $$Ifa$gdFf9' $$Ifa$gdi $Ifgd8 $$Ifa$gd+tV>X>kd)$$Iflִ=z*0 ==XXX0    4 lalX>b>l>v>>>>>>>>>>>>>>>>???? 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$IfgdZ"kd5$$Ifl\: ` R t044 la $$Ifa$gdSha $$Ifa$gdZ"FFFFF $$Ifa$gdSha $$Ifa$gdZ"FFFRGG:111 $IfgdZ"kd5$$Iflֈ` 8:(R t044 laGGGGHH HHHH%H*H1H}qqqqqqqqqq $$Ifa$gdco $IfgdZ"ykd6$$Ifl0: t044 la 1H2H8H>HHH:1111 $IfgdZ"kdk7$$Iflֈ iQ: t044 laHHHHHHHHHHHHH}qqqqqqqqqq $$Ifa$gdco $IfgdZ"ykdR8$$Ifl0: t044 la HHHHHHHHxIyIJ:<>JNtv"(*ܼ޼npvзЋzn`nhUMh[_6H*mHsHhUMh[_6mHsHh H*mHsHh mHsHh[_mHsHhUMhv9$6mHsHhUMhN6mHsHhUMh %6mHsHhX@6mHsHhNmHsHhv9$mHsHh %mHsHhX@mHsHhVUh<_ h<_CJ h&5Hh&5Hh&5Hh&5HH*"HHHHHHHHHHHIIIIIII#I'I,I0I5I9I>I?IFfr@Ff*= $$Ifa$gdco $IfgdZ"Ff9?ILIOITIWI\I`IeIiInIrIwIxIyI:<vgd[_$a$gd<_$a$gdjUFfC $$Ifa$gdco $IfgdZ"akovo and the SF Kutjevo  Table 4). However, the higher position of the SF  Kutjevo (area of Pozega municipality: about 250 m above sea level = ASL) is more favorable for maize growth under water shortage conditions (the lower temperatures) in comparison with lowland position of akovo area (between 110 and 150 m ASL). This phenomenom could be used as explanation for maize yield reduction (comparison favorable 1991 and unfavorable 1992 growing season) for only 25% in the SF Kutjevo compared to 49% in the SF akovo (Table 4). Table 4. Weather characteristic influences on maize yields on two state farms of Eastern Croatia* for two growing seasons (1991 and 1992)  Kova evi, 2004) Tabela 4. Uticaj vremenskih prilika na prinose kukuruza na dva kombinata isto ne Hrvatske* za dve godine (1991 i 1992)  Kova evi, 2004) Precipitation (mm) and mean air-temp. (0C) for two growing seasons Koli ina oborina (mm) i srednje temp. zraka (0C) za dvije vegetacijeMonthakovo Weather BureauKutjevo Weather BureauMesecMeteoroloaka stanica akovoMeteoroloaka stanica Kutjevo1991199219911992mm0Cmm0Cmm0Cmm0CMay June July August Sept.112 34 152 50 2212.5 20.0 22.0 20.5 17.846 111 27 20 2917.0 19.5 21.0 25.3 18.072 90 82 78 5811.7 18.5 20.8 19.4 16.9 113 56 14 24 18.8 20.3 23.5 16.7Sum370233380266Mean18.620.217.418.9Mean yields of maize (t/ha) / Prose ni prinosi zrna kukuruza (t/ha)State farm Djakovo / PIK akovoState farm Kutjevo / PPK Kutjevo8.134.168.516.41Index1005110075* Remark: soil characteristics of both state farms are mainly similar * Napomena: karakteristike zemljiata na obadva kombinata su uglavnom sli ne Water deficite became main limiting factor of maize yields in Eastern Croatia under dry farming system (without application of irrigation). Irrigation in the critical stages of maize growth under water deficite stress is solution for stabilization of maize yield variations among years and their lower dependences on precipitation and temperature regimes. REFERENCES Janekovic Gj. (1971): Pedologic characteristics of Slavonia and Baranya (in Croatian with English abstract). Zbornik radova Prvog znanstvenog sabora Slavonije i Baranje, 17-19. svibanj 1970, Osijek , p.115-176. Josipovi M., Kova evi V., Petosic D. and `ostari Jasna (2005): Wheat and maize yield variations in the Brod-Posavina area. Cereal Research Communications 33 (1):229-233. Kovacevic V. , Kaucic D. (2006): Weather characteristics impacts on yields of the spring crops in Croatia. In: Proceednings, 41 Croatian & 1st International Symposium on Agriculture, (S. Jovanovac and V. Kovacevic Eds.), 13-17. February 2006, Opatija, Croatia, Faculty of Agriculture, University J. J. Strossmayer in Osijek, p. 421-422. Kova evi V., `imi D., `oatari J., Josipovi M. (2007): Precipitation and temperature regime impacts on maize yields in eastern Croatia. Maydica 52 (in press). Lang I., Farago T., Ivanyi Z. (Editors), (2006): International Conference on Climate Change  Impact and Responses in Central and Eastern European Countries 5-8 November 2005, Pecs, Hungary. Hungarian Academy of Sciences, Hungarian Ministry of Environment and water, The Regional Environmental Centre for and Eastern Europe. Petosic D., Kovacevic V., Josipovic M. (2003):Phosphorus availability in hydromorphic soils oh Eastern Croatia. Plant, Soil and Environment 49 (9): 394-401. Shaw R. H. (1988): Climatic requirement. In: Corn and corn improvement, Agronomy Monograph No 18 ( Sprague G.F. ed.) ASA-CSSA-SSSA, Madison, Wisconsin, USA, p. 609-638. `koric A., Filipovski P., Ciric M. (1985): Klasifikacija tala Jugoslavije, ANU-BiH, Sarajevo. `oatari J., Josipovi M. (2006): Weather and soil influences on maize yield in the Eastern Croatia. Universitatea se Stiente Agricole si Medicina Veterinara Iasi, Lucrari Stiintifice  Volume 49, seria Agronomie, p. 375-381. UTICAJ PADALINA I TEMPERATURA NA PRINOSE KUKURUZA U ISTO NOJ HRVATSKOJ Rezime Kukuruz je s 0.4 miliona hektara ili oko etvrtinu ukupnih oranica najrasprostranjenija ratarska kultura na oranicama Hrvatske. Openito, postoji uska veza niskih prinosa kukuruza s deficitom padalina i viaim temperaturama vazduha. Dve godine (2000. i 2003.) bile su naro ito nepovoljne za kukuruz. Tako je u 2000. g u isto noj Hrvatskoj ostvaren za 34% ni~i nego u prethodne etiri godine uglavnom zbog manjka padalina. U 2003. g su niski prinosi kukuruza bili u vezi sa suaom u junu i avgustu (30% manje kiae) i visokim temperaturama vazduha  prosjek 23.3 oC ili za 2.8 oC viae od 30-god. prosjeka. Suaa postaje sve vei faktor ograni enja prinosa kukuruza u isto noj Hrvatskoj. Tema ovoga rada je utvrditi vezu izmeu ptrinos akukuruza i vremenskih prilika. Navodnjavanje je potrebno da bi se smanjilo variranje ptrinosa kukuruza po godinama. 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