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1 PRO GR ESS IN GEO GRA PH Y V o l. 20, N o. 4 D ec., 2001 : (2001) , (, ) :, 501 mm 502 mm, m m 3, m 3,,, ;, : ; ; : P42616; P343 : A 1 (IGBP) - [1 ] (BA HC), 21, IGBP (973 ),,,, km 2,?,, : ; : : (G , G ); (g 29903) : (19652 ),,,, IGBP 2001 :

2 [2, 3 ], 450 mm, m mm 502 mm m m 3, m 3,,,,,,,,,,,??, 3 311,,,,,,,,,,, [4, 5 ], km 2,,, [4 ],,,, 0135,

3 4 : ,,, 312,,,,,,,,,,,,,,,,,, km 2, 97% :, 1 1 Tab11 Prec ip itation and runoff amoun t in typ ical years of Y ellow r iver basin gmm g10 8 m 3 gmm g10 8 m 3 gmm

4 :,,,,,,, ; >, > , 2 2 Tab12 Prec ip itation- runoff relation in var ious section s in the Y ellow R iver Basin Y = X R 2 = Y = X R 2 = Y = 01019X R 2 = Y = X R 2 = Y = X R 2 = Y = X R 2 = , Y, X, mm R 2,, R 2 015,, R 2 017,,,,,,, m 3, m 3, 20%,,, 2 3 mm,,, m 3, m 3, 3% 3, 43 mm, mm, m 3, m 3, m m 3, m 3, m 3,, m 3, m 3, m 3, m 3,

5 4 : m 3, m 3,,,,, 314 ( km 2 ),, 3 3 Tab13 Observed Prec ip itation and runoff amoun t in upper Lanzhou reg ion ( ) ( ) ( ) ( ) ( ) gmm g10 8 m g10 8 m 3 gmm : 3, g10 8 m g10 8 m (, 3 ) km km mm, 565 mm, m mm, 339 mm, m 3, 443 mm, 493 mm,,, m 3,

6 360 20,,,,,,,,, 315,,,, 4 4 Tab14 Prec ip itation- runoff relation dur ing f lood per iod and non-f lood per iod in var ious section s of Y ellow r iver - Y = 01396X R 2 = Y = 01246X R 2 = Y = X R 2 = Y = X R 2 = Y = X R 2 = Y = X R 2 = Y = 01181X R 2 = Y = X R 2 = Y = X R 2 = Y = X R 2 = Y = X R 2 = Y = X R 2 = ,,,,,,,,, 4, ,,,, ;,,,

7 4 : ;,, ;,,, ;,,, :,, 5, m 3,,,,,,,, : [ 1 ],. () [J ]., 2000, 19 (2) : [ 2 ],. [M ]. :, , [ 3 ],. [M ]. :, [ 4 ]. [M ]., [ 5 ],,. [M ]. :,

8 A Research of the Im pacts of Uneven Prec ip itation on the Natural Runoff in the Y ellow R iver ZHAN G Sh i2feng, J IA Shao 2feng ( Institute of Geograph ical Sciences and N atural R esources R esearch, CA S, Beijing , Ch ina) Abstract: T he impact of uneven p recip itation on the runoff amoun t is very sign ifican t in the Yellow R iver basin. T he years of and are bo th rich hydro logical years w ith p recip itation of 501 mm and 502 mm, respectively, bu t the natu ral runoff amoun ts of the tw o years at the H uayuankou station are 7615 and 6318 b illion m 3. T h is m ean s that there is a 1217 b illion s m 3 difference of runoff amoun t w hen the rainfalls are almo st the sam e. T h is paper analyzes the impact of p recip itation unhomogeneity on runoff generation. F irst2 ly, the impact of spatial unhomogeneity is analyzed. T he no rm al m ethod is to divide the Yellow river basin in to five section s, nam ely, upper L anzhou section, L anzhou- H ekou section, H ekou - L ongm en section, L ongm en - Sanm enx ia section, Sanm enx ia - H uayuankou section. W hen w e analyze by u sing th is division, the sim u lation resu lt in the fou r section s of low er L anzhou region is qu ite good, bu t the sim u lation resu lt in upper L anzhou section is bad. Concretely, the sim u lation resu lt is that the runoff amoun t in is 617 b illion m 3 mo re than that of in the m iddle reaches, w h ich is very clo se to the m easu red 514 b illion m 3. A nd the resu lt also show s that the reason of the difference of the runoff am oun t genera ted in the m idd le reach is tha t the p recip ita t ion and runoff in the L ongm en- Sanm enx ia section is differen ṫ In the L anzhou- H ekou section, the difference of p recip itation doesn t impact the runoff very sign ifican tly since the p recip itation- runoff generation coefficien t is very sm all. T he runoff amoun t generated in th is section is very sm all. T he p recip itation and runoff in the H ekou - L ongm en section and Sanm enx ia - H uayuankou section are differen t bu t to tal amoun ts are very clo se. T herefo re the reason fo r the difference of w ater amoun t is the runoff generation in the upper L anzhou section and L ongm en- Sanm enx ia section. A cco rding to sim u lation resu lt th rough the p recip ita2 t ion - runoff rela t ion, the p recip ita t ion and runoff am oun t in is less than tha t of, bu t the m easu red figu re of p recip itation in is less than that of w h ile the runoff in is 715 b illion m 3 mo re than that of. T h is m ean s that the no rm al divi2 sion can no t exp lain the runoff generation characteristics. T hen w e m ake fu rther division of the spatial scale by subdivision of upper L anzhou section in to upper T angnaihai section and T angnaihai- L anzhou section. T he resu lt is that, although the p recip itation of upper L anzhou section of is less than that of, the p recip itation and runoff of upper T angnaihai section of are larger than tho se of, and the p recip itation and runoff

9 4 : 363 of T angnaihai- L anzhou section of keep less than tho se of, w h ile th is upper T angnaihai section is the so- called h igh w ater generation rate section. T h is resu lt can ex2 p lain w hy the runoff of upper L anzhou section in is larger than that of w h ile the p recip itation of upper L anzhou section in is less than that of. Such a subdivision can clearly indicate that the p recip itation and runoff relation in upper T angnaihai section is dom inan t in the upper L anzhou sction. T herefo re spatial division m u st be draw n in to T angnaihai section at least, and the resu lt cou ld exp lain the p recip itation- runoff relation. Secondly, w e subdivide the tempo ral scale in to flood period and non2flood period. A nalysis resu lt show s that such a tim e scale division doesn t impact very m uch of p recip itation - runoff relation and that, at the verse, the sim u lation resu lt of p recip itation- runoff rela2 tion is w o rse than that in year- scale. Key words: p recip itation unhomogeneity; Yellow R iver; natu ral runoff

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