Mj. Salinger et Gj. Kenny, CLIMATE AND KIWIFRUIT CV HAYWARD .2. REGIONS IN NEW-ZEALAND SUITED FOR PRODUCTION, New Zealand journal of crop and horticultural science, 23(2), 1995, pp. 173-184
Matching crops to climate is an important activity for planning produc
tion. Three important climatic factors were identified as being import
ant determinants of kiwifruit (Actinidia deliciosa 'Hayward' (A. Chev)
C.F. Liang et A.R. Ferguson) distribution: winter chilling; growing s
eason thermal time; and annual rainfall. Indices for each of these fac
tors were developed to enable mapping of the most suitable areas for k
iwifruit production. These were May-July temperatures of 11 degrees C
or less as the optimal winter chilling requirement, a thermal time acc
umulation of 1100 degree-days above 10 degrees C from October to April
, and an annual rainfall of 1250 mm or more. Apart from Northland, all
the traditional areas of kiwifruit production have a suitable climate
. However, there are substantial areas of inland Bay of Plenty to Roto
rua, the Waikato, north Taranaki, and northern Hawke's Bay where the c
limatic requirements are also satisfied. A high frequency of extreme w
inds may be an additional limiting factor in some of these regions, su
ch as Taranaki. The total area of suitability is enlarged if irrigatio
n is available, particularly in the southern North Island and central
Marlborough. Within this climatic range the estimated dates for the av
erage end of dormancy and 50% flowering are spread over 4 weeks, and e
stimated budburst dates over 11 days. Although use of average climate
data to describe kiwifruit distribution provides a valuable first-orde
r assessment, it would be desirable to incorporate analyses of climate
variability in future studies of this kind.