ISRAEL JOURNAL OF
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VETERINARY MEDICINE home archive journal |
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Vol. 56 (3) 2001 |
THE
INTERACTION BETWEEN CLIMATIC FACTORS AND BLUETONGUE OUTBREAKS IN ISRAEL AND THE
EASTERN MEDITERRANEAN, AND THE FEASIBILITY OF ESTABLISHING BLUETONGUE-FREE ZONES |
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Y.
Braverman1, F. Chechik2, B. Mullens3
1. The
Kimron Veterinary Institute, Bet Dagan, Israel; 2. The
Meteorological Services, Bet Dagan, Israel; 3.
Department of Entomology, University of California, Riverside, CA, USA |
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Abstract Israel has
accumulated extensive information on bluetongue (BT) occurrence in sheep flocks
and sentinel cattle in various regions of the country for more than 30 years.
Meteorological parameters had not been independently correlated with the
occurrence of BT over the entire period. Meteorological parameters preceding
years with high prevalence of bluetongue (1975, 1987, 1988 and 1994) (average of
43 sheep flocks affected) were compared with those for years with little or no
BT transmission (1980, 1981, 1983 and 1992). Winters preceding high-BT seasons
were significantly warmer; the average maximum temperature of the coldest month
was 2 to 30C higher, and the average
maximum and minimum temperatures were 1-20C
higher. After extremely dry and warm winters over the eastern Mediterranean,
such as those of 1998 and 1999, single cases of BT occurred in 1998 and none in
1999. Rainfall in BT outbreak years was approximately normal, whereas winters
preceding low-BT seasons were wetter (40% more rainfall than average in the
coldest month and 17% more winter rainfall overall). BT outbreak years had
significantly more winter days with maximum temperatures higher than 13 or 180C (in the Inner-land and in the Arava
regions, respectively), and more nights with minimum temperatures > 50C. Average maximum temperatures below
16.50C for the coldest winter month were
associated with low-BT seasons, while winters with more than 18 days warmer than
180C were followed by high BTV
transmission. In most parts of Israel except in mountains >700 m above sea
level, the average maximum temperature of the coldest winter month is >12.50C, which is thought to enable the
survival of BT viruses. Mountain areas also have fewer animals/km2 than lowland areas, and more of these
are BT-resistant ruminants such as goats. Two candidates for "safe
zones" with regard to export of ruminants and their products are proposed:
the Arava Rift Valley and mountains above 700 m. Bluetongue outbreaks are not
known in these regions. The Arava is assumed to be a particularly low-risk
region because there are smaller numbers and presumed lower survival of the
principal vector, Culicoides imicola. The Arava Rift Valley is also
beyond the Persian Trough air stream, which seems to be connected with the
introduction of BT vectors into Israel. These safe zones might be exploited for
export of animals and germplasm. |
Introduction Materials and Methods Results Discussion Tables
Bluetongue
(BT) disease affects wild and domestic ruminants and is widely distributed
globally. Biting midges of the genus Culicoides transmit bluetongue
viruses, and the distribution and abundance of the vector are thought to account
for the seasonal and spatial distributions of BT (1). Several attempts have been
made to relate climatic factors to outbreaks and spread of BT in various regions
(2, 3, 4). Walker and Davies (5) found in Kenya that numbers of several dominant
Culicoides species, including the principal vector C. imicola (=pallidipennis)
greatly increased after the rainy season. They postulated a causal relationship
between peak rainfall in April-May, peak numbers of Culicoides in
May-June and peak bluetongue prevalence in June-July. However, Davies (6) did
not find that rainfall affected serological conversion rates of sentinel cattle
to BT viruses in Kenya. Wright et al. (4) related weather variables to
seroconversion in cattle to bluetongue in Alabama, USA; while the best
predictors were mean daily hours of wet vegetation (as the result of dew) and
total rain days during the second weekly period prior to sample collection. The
most thorough studies have been done in Australia, where Ward (3) studied 18
climatic variables: Daily maximum temperature and average annual rainfall best
explained the variability in the prevalence of BT. Subsequent modeling efforts
(7) showed that spring rainfall and minimum temperatures had the greatest
effects on predicted transmission; periodic disruptions (drought) introduced
cyclic instability into the model, mirroring patterns that are sometimes seen
naturally.
Movement of
Culicoides species in Australia has been associated with northerly winds
(8) and that in Israel with a summer north-westerly wind system termed the
Persian Trough (9). Most outbreaks of BT in Israel occur from mid-summer (July)
to the onset of cold winter temperatures (November-December) paralleling the
activity of the Persian Trough and the buildup of large numbers of C. imicola
vectors (9) with high vectorial capacity (10, 11). Similar climatic factors
prevail over the eastern Mediterranean, and the situation in Israel should be
representative of this area. The present study was undertaken to elucidate which
climatic factors, or combination thereof, determine BT prevalence in Israel. We
also investigated whether BT-free zones might exist in Israel.
Data on BT
outbreaks in sheep flocks were available from the Epidemiological Quarterly of
the Israeli Veterinary Services. Climate data were obtained from the Israeli
Meteorological Service. The rainfall data were regional averages taken from 22
meteorological stations (Table 1) whose distribution was related to the size of
the BT-affected area. i.e., more meteorological stations were included for a
larger affected area than for a smaller affected area. Data characterizing
winter frost days and spring Sharav days (Sharav day=a day with maximum
temperature of 330C or more, and relative humidity
at 1400 h of 25% or less) were taken from the Kefar Blum meteorological station,
where the probabilities for frost and Sharav days are high. This northern
locality is representative of the climate of the inland valleys.
Two types
of analyses were conducted: linear correlations between BT outbreak frequencies
in sheep flocks versus selected climatic factors; and climatological comparisons
of years with many BT outbreaks (> 30) versus years with 0 to 1 BT outbreak.
Correlations were examined between BT outbreak frequencies (number of outbreaks)
and climatic data over a 20-year period (1970-1989). The following climatic
factors were tested: 1. Seasonal (September-May) rainfall (mm); 2. Spring
(March-May) rainfall (mm); 3. Number of nights between November and March during
which the minimum temperature was <50C; 4. Number of frost nights
(November-March); 5. Number of consecutive frost nights (November-March); 6.
Number of consecutive nights (November-March) with temperature of 20C and below; 7. Number of spring
(April-May) Sharav days; 8. Number of spring days with maximum temperature of 350C and above; 9. The highest daily
maximum temperature of the year. A detailed analysis was done, to compare
climatic factors prevailing before each of four years with many BT outbreaks
(>30) (1975, 1987, 1988 and 1994) versus climatic factors for four years with
0-1 BT outbreaks (1980, 1981, 1983 and 1992). The values of each climatic factor
in low-BT and high-BT years were compared by t-test. It was assumed that extreme
temperatures (very low or very high) and drought prevailing in a certain year
would reduce the number of surviving vectors in the following year. Data for
this analysis were taken from two meteorological stations: Kefar Blum in the
north and Bet Dagan on the central coastal plain, where the frequency of frosts
and Sharav days is lower than in Kefar Blum. For each of the four-year
groupings, the following averages of meteorological parameters were tested: 1.
Average maximum temperature (0C) of the coldest winter month (December-March); 2. Average maximum
winter temperature; 3. Minimum winter temperature; 4. Number of days with
maximum temperature of 130C or above in January-February;
5. Number of days with maximum temperature of 180C or above in January-February; 6. Number of winter (December-March)
nights in which the minimum temperature was 50C or below; 7. The average amount of rainfall at 22 meteorological
stations; 8. Spring (April 1 to June 15) maximum temperature; 9. Number of
Sharav days in the spring (March-May); 10. The average amount (mm) of spring
rainfall as measured at 22 meteorological stations.
Culicoides trapping: Where data were available, the
numbers of Culicoides at the various localities were related to specific
regions or seasons. Collections were made in DuToit suction light traps (12)
equipped with mercury vapor lamps (HPW125 W-TS, Belgium). Bet Dagan, in the
central Coastal Plain served as a permanent trapping station, where Culicoides
were collected either throughout the summer or throughout the year. Collections
at Bet Dagan were made at the byre of the Veterinary Institute, the byre of the
Volcani Center, or at both sites. At Bet Jann, Upper Galilee, 36 suction light
trap collections were made between August 25 and October 6, 1981. At En Kerem in
the Judean Hills, 30 suction light trap collections were made between September
and December 1978. At Yotvata in the Arava Valley, two suction light trap
collections were made in August 1982.
Introduction Materials and Methods Results Discussion Tables
The average
maximum temperatures of the coldest month (usually January) in Israel are shown
in Fig. 1. Temperatures between 12.5 and 180C, which are thought to enable the
survival of BT viruses in vectors during winter (13) prevail over most of the
country. The exceptions are hills above 700 m (<12.50C) and the Arava and Jordan Valley
(>180C). There was no correlation between
the 10 individual climatological parameters and the numbers of BT outbreaks in
sheep during 1970-1989 (Table 2). Temperatures in the four winters that preceded
seasons with many outbreaks and those that preceded seasons with no (or few)
outbreaks are shown in Table 3. Seasons with many outbreaks were preceded by
winters in which the average maximum temperature of the coldest month was 2 to 30C warmer (P=0.0009). In addition
the average maximum and the average minimum temperatures of the entire winter
(December-March) were 1 to 1.50C
warmer in winters preceding high-incidence years (P=0.0061). High-incidence
years were preceded by winters (January-February) with more days in which the
maximum temperature was > 130C (P=0.0346) and >180C (P=0.0002). The number of spring
Sharav days was not useful to distinguish high-incidence from low-incidence
years. Low incidence years were preceded by wet winters, with 40% more rainfall
on the average of the coldest month than those which preceded by high-incidence
years (and which had approximately normal rainfall) (P=0.0058). The overall
amount of rainfall in years without outbreaks was, on average, 17% higher than
that in years with many outbreaks. The data of Table 3 indicate that average
maximum temperatures below 16.50C in the coldest month of winter
were associated with a low probability of BT outbreaks in the following summer.
Likewise, winters with more than 18 days with temperatures above 180C were associated with a high
probability of BT outbreaks in the following summer. The mountains (700 m above
sea level) had no reported BT outbreaks, and the Arava desert valley (e.g.,
Yotvata, 75 m above sea level) recorded only a single BT case during 1970-1989.
These areas have fewer Culicoides vectors than a typical BT area such as
Bet Dagan (Table 4). Table 5 shows the numbers of vectors, namely C. imicola,
trapped in June, one month before the usual outbreaks of BT in sheep. There were
large differences in the numbers of Culicoides spp. at the two
sites at Bet Dagan and between the numbers collected in 1982 and in 1996. In the
absence of a source of infection, even a C. imicola population yielding
345 insects per night per trap at the Volcani Center in 1982 did not result in a
BT outbreak (Table 5). Table 6 shows the numbers of Culicoides spp.
trapped nightly during the BT-free season, i.e., winter of 1997/8. The numbers
of the vector C. imicola ranged from 170 in November 1997 to 6 in
February and March 1998. The Rehovot District (Fig. 2), which includes Bet
Dagan, contains large numbers of reservoir animals, i.e., dairy cattle, it is
not surprising therefore that the BT virus is active in this area. In contrast
parts of the Be'er Sheva District, which includes the flat Arava, and the
Jerusalem and Akko Districts, which are hilly and contains smaller numbers of
cattle that may serve as BT reservoirs.
Introduction Materials and Methods Results Discussion Tables
Climatic
variables presumably influence BT spatial and seasonal distributions through
modifications of vector capacity and abundance. Vector capacity incorporates
biting rates, vector survival, extrinsic incubation (time required between
ingesting the virus and becoming infective), and vector competence (ability of
the vector to become infected by the virus). Our analysis concentrated more on
winter climate parameters than on summer ones, since in the eastern
Mediterranean summer parameters are stable whereas the winter ones are variable
(14, 15). The importance of winter was confirmed in a recent study in Spain,
where it was reported that C. imicola predominated in a zone with the
highest minimum and maximum temperatures during the winter (16). Both
temperature and rainfall appear to be significant.
Temperature: Temperature has a profound influence
on several of these vector capacity components. Our temperature analysis shows
that, theoretically, BT virus types should be able to survive the winters, at
least in part, in infected insects throughout the entire country, except in the
mountains above 700 m. Extrinsic incubation of BT virus in the vectors is
temperature dependent: in the laboratory, C. sonorensis, BT virus
remained in a quiescent state for at least 22 days, but it replicated rapidly
when infected insects were exposed to higher temperatures (17). The virus is
assumed to survive above a temperature threshold of 12.50C (13), which is below the activity
threshold for flight of C. imicola. While C. imicola may be
collected on warm winter evenings, its minimum temperature for flight is 17-180C (18). It has been suggested in other
subtropical areas that are within its wide range, that winter persistence of
infected C. imicola provides at least a partial means of over-wintering
for BT viruses (19, 20).
Developmental
rates, and, therefore, the generation interval of a multivoltine insect such as C.
imicola, are considerably shorter at higher temperatures (see, e.g., 21),
which might enable population densities to increase more quickly. In winter
larvae of C. imicola do not hibernate, but develop at a slower pace, so
that higher winter temperatures might lead to a larger spring generation. The
length of the gonotrophic cycle, particularly the time required from blood
ingestion to egg development, is also much shorter at higher temperatures,
provided they are below the upper threshold limits (22). Thus individual vectors
should feed more often, increasing opportunity for transmission over a defined
time period. These factors would act to encourage BT activity at higher
temperatures. Indeed Rawling et al. (23) suggested that the presence of
C. imicola in Iberia is favoured by high summer temperatures, possibly in
conjunction with the seasonal low relative humidity. No significant
relationships between the presence of C. imicola and winter temperatures
and relative humidity were found. On the other hand, it is expected that daily
survival would be lower at higher temperatures, such as those prevailing in the
Arava. The fact that the preferred climatic conditions for reaching peak
populations of C. imicola always occur everywhere in Israel in the autumn
(September- November), when night temperatures are lower and relative humidity
is higher than in the summer, reflects a different situation from that in Spain
(23). The prevailing high winds in the Arava probably regularly suppress the
host-seeking activity of C. imicola and increase their mortality, as was
suggested previously (24, 25). However, Braverman et al. (11) found that C.
imicola collected in light traps in the Coastal Plain, where temperatures
are more permissive maintained a high parity level (stage survival) during the
mid summer and early fall months. Survival between blood meals was actually
highest in August on the Coastal Plain (Bet Dagan).
Our
analysis suggests that warm winters, which encourage survival in C. imicola,
precede periods of substantial BT transmission. This could be a result of
reduced mortality and higher overwintering populations of the vector but, except
for the Bet Dagan area, we lack concurrent long-term vector monitoring data to
substantiate this. The above suggestion does not mean that BT outbreaks will
actually occur after every warm winter; the very dry and warm winters of 1998
and 1999 were followed by summers with few BT outbreaks only in 1998. C.
imicola is essentially an African species, more adapted to high temperatures
than low ones. Warm spring Sharav days had no detectable influence on BT
occurrence, probably because winter-induced C. imicola mortality had
already occurred and preceded the Persian Trough air stream that starts in the
2nd half of June and is believed to introduce BT-infected vectors (9).
Rainfall: Because the immature stages of C.
imicola are found in areas of damp or wet manure/organic soil, one might
assume that rainfall would have a major positive influence on vector population
densities. A recent study used the Normalized Difference Vegetation Index
(NDVI), a satellite-derived measure of photosynthetic activity, to evaluate
relative abundances of C. imicola (24). Abundances were positively
correlated with the average and minimum NDVI (NDVImin), an index which is
strongly correlated with total annual rainfall. In the eastern Mediterranean the
rainy season is limited to the winter, and our analysis suggests that very wet
winters result in reduced BT transmission the following summer. An important
reason for this is that heavy rains inundate and erode the breeding sites of C.
imicola. Ample rainfall-independent development sites for C. imicola are
found near water troughs, etc., in and around livestock yards (26, 27). Unlike
the situation in Morocco and Iberia (24) grass-covered wet sites were found to
be poor biotopes for C. imicola. Irrigated fields and horticultural crops
in Israel are also not dependent on rainfall, and provide breeding sites for C.
schultzei gp. and other species (not C. imicola). The negative
influence of rainfall is more likely due to the fact that wetter winters are
also much cooler, which may reduce vector survival. A contradictory phenomenon
was found in South Africa regarding C. imicola and African horse sickness
(AHS) outbreaks. It was found that a spell of drought succeeded by heavy
rainfall was followed by AHS epizootics (28).
Wind
patterns: It is as yet unclear to what
extent the BT virus overwinters in vectors in Israel, as opposed to
overwintering in vertebrate reservoirs, exploiting seasonal animal movement
(limited to the Bedouin's flocks, who raise non-susceptible animals), or
potential seasonal introduction via airborne vectors. The local air stream in
the Arava valley flows from the Dead Sea southward through the Red Sea region.
Constant winds between 20:00 and 23:00 h have a velocity of 15 km/h, and this
might actually suppress flight activity, prevent biting during the main feeding
hours and result in increased mortality of C. imicola (25, 29). The
detrimental effects of high wind speeds on C. imicola are due to
desiccation, prevention of feeding and physical removal. High wind speeds have
the potential to move insects considerable distances quickly, but this is
difficult to demonstrate. Despite this, one may consider the potential influence
of the air stream on vector introduction into the two candidate regions we
propose as BTV-free zones.
Candidate
bluetongue-free zones:
Based on historical BT records, the disease is basically unknown in two regions
of Israel-mountainous areas and the Arava Desert (30). Mountainous regions above
700 m, although in the path of the Persian Trough airstream (15), have several
characteristics that suggest they will remain BTV-free for at least the near
future. First, numbers of C. imicola are relatively low, and substantial
overwintering is unlikely. Animal densities are relatively low (Fig. 2), and
species composition is dominated by goats, mainly of the Mamber breed, and local
sheep breeds, mainly Awassi, which are fairly resistant to BT (31, 32) and are
not preferred hosts for the vector, C. imicola (33). This area is likely
to remain BT-free until more susceptible ruminants are introduced. Higher
standards of living might result in the introduction of more cattle and European
sheep breeds, which could, in turn, result in more BT transmission. This would
be especially true for dairies, which provide disproportionately suitable
developmental sites for the vector. The Arava Desert also has a relatively small
number of C. imicola. The growing numbers of dairies in this area are
likely to increase vector numbers, but very high summer temperatures also should
result in poor survival of the vectors and thus maintain low vector capacity
(11, 36). The Arava Desert should be investigated thoroughly to check whether it
is a valid BTV-free area. The indication of probably being BTV-free is supported
by the fact that in the Southern Arava serological survey in sentinel cattle
showed that they have been free of BTV at least 13 years (30). However, this
region may also serve as a source of C. imicola innoculum for more
northerly regions in spring and early summer, particularly after winter
mortality in those cooler climates, and given the prevailing wind patterns. The
density of C. imicola in the Arava will rise with the growing numbers of
new dairies there but, as the Arava is beyond the Persian Trough system (15) and
because of the supraoptimal temperatures prevailing in the summer, the survival
of the C. imicola population may be too low for transmitting BT (11, 36).
Probably an additional limiting factor, for the survival of C. imicola at
present is the scarcity of carbohydrate sources. This might change as the areas
of irrigated crops and trees increase in the future. Therefore, the Arava should
be considered as a probable BT-free safe zone, at present.
Routine
monitoring of the vector C. imicola is advisable, particularly near
animals, in these proposed BTV-free zones. Trap collections are highly variable
and, therefore, must be interpreted cautiously. On the assumption that light
trap collections in some way approximate biting rates, it is possible
approximately to relate collections to risk, pending more definitive research.
Holbrook (35), for example, reported no observed BT transmission to sentinel
sheep at light trap collections below ca. 35-40 C. sonorensis
females/trap. From our extensive observations at Bet Dagan, where BT often
occurs (but seasonally), DuToit light trap collections in cow sheds of ca. 345
C. imicola or above tend to be associated with BT outbreaks. If vector
populations of such magnitude exist in an area when BT viruses are introduced by
some means, substantial transmission might be expected. In simulation studies of
African horse sickness in Spain, it was found that during an outbreak the
proportion of infected C. imicola never exceeded 3% and that below a
threshold of ca. 11,000 C. imicola per host no outbreaks occurred (23).
Further studies would be useful to refine this rough figure and relate it to
specific fluctuations in vector capacity components.
Acknowledgements
We are
obliged to Dr. E. Rapaport of the Veterinary and Animal Health Services, Afula
for providing the data on outbreaks of BT in sheep, to Dr. A. Gnizi and Mrs M.
Zarchi of the Volcani Centre for performing the statistical analysis and to Dr.
M. Van Ham of the Israeli Veterinary and Animal Health Services, Bet Dagan for
providing the figures on farm animal abundance in the various districts.
Introduction Materials and Methods Results Discussion Tables
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Braverman, Y., Boreham, P.F.L. and Galun, R.: The origin of blood meals of the
female Culicoides pallidipennis trapped in a sheepfold in Israel. J. Med.
Entomol. 8: 379-381, 1971.
34. Lord,
C.C., Woolhouse, M.E.J. and Mellor, P.S.: Simulation studies of African horse
sickness in Spain. Arch. Virol. (Suppl) 14: 103-111, 1998.
35.
Holbrook, F.R.: Research on the control of bluetongue in livestock by vector
suppression. In: Barber, T.L., Jochim,
M.M. and Osburn, B.I. (eds.):
Bluetongue and Related Orbiviruses. Alan R. Liss, Inc. New York. pp. 617-620,
1985.
36. Wellby,
M.P., Baylis, M. Rawlings, P. and Mellor, P.S.: Effects of temperature survival
and rate of virogenesis of African horse sickness virus in Culicoides
variipennis sonorensis (Diptera, Ceratopogonidae) and its significance in
relation to the epidemiology of the disease. Bull. Entomol. Res. 86: 715-720,
1996.
Table 1 Table 2 Table 3 Table 4 Table 5 Table 6
Introduction Materials and Methods Results Discussion Tables
Table
1: Stations from which precipitation
data were taken for the BT study
|
Locality |
Altitude above ground
(m) |
Latitude N' |
Longitude E' |
|
Akko |
15 |
320 55' |
350 05' |
|
Ein haHorsh |
18 |
320 23' |
340 56' |
|
Galed |
180 |
320 33' |
350 04' |
|
Ma’abarot |
20 |
320 22' |
340 54' |
|
Bet Dagan |
30 |
320 00' |
340 49' |
|
Yavne |
20 |
310 54' |
340 46' |
|
Qiryat Eqron |
50 |
310 52' |
340 48' |
|
Elon |
300 |
330 03' |
350 13' |
|
Moshav Meron |
941 |
330 00' |
350 23' |
|
Nazareth-Elit |
460 |
320 42' |
350 19' |
|
Ramat David |
80 |
320 41' |
350 12' |
|
Mizra |
99 |
320 40' |
350 17' |
|
Afula |
60 |
320 36' |
350 17' |
|
Tavor |
145 |
320 41' |
350 24' |
|
Atarot |
757 |
310 52' |
350 13' |
|
Kibbutz Hazerim |
190 |
310 13' |
340 36' |
|
Beer Sheva |
280 |
310 15' |
340 48' |
|
Golan Exp. Station |
940 |
330 07' |
350 48' |
|
Gadot |
100 |
330 01' |
350 37' |
|
Kefar Blum |
75 |
330 10' |
350 36' |
|
Deganya Alef |
-200 |
320 43' |
350 34' |
|
Tirat Zevi |
-220 |
320 25' |
350 32' |
Table 1 Table 2 Table 3 Table 4 Table 5 Table 6
Introduction Materials and Methods Results Discussion Tables
Table 2: Coefficient of correlation between
number of BT outbreaks in sheep flocks in Israel in the years 1970-1989 to
selected climatic factors at Kefar Blum
|
Meteorological parameter |
Coefficient of the linear
correlation |
|
*Amount (mm) of rainfall, September
through May |
0.063 |
|
*Amount (mm) of spring (March-May)
rainfall |
-0.240 |
|
Number of frost nights (<00C) between November and March |
0.154 |
|
Number of consecutive frost night
between November and March |
0.154 |
|
Number of consecutive nights in
which the minimum temperature |
|
|
was ²2 0C between November and March |
0.070 |
|
Number of nights between November
and March in which the |
|
|
minimum temperature was ²50C |
-0.052 |
|
The winter minimum temperature
between November and March |
-0.118 |
|
Number of Sharav days in spring
(April 1 through June 15) |
-0.136 |
|
Number of days in the spring in
which the maximum temperature was >35?C |
0.099 |
|
The annual maximum temperature |
-0.441 |
*Average from 22 meteorological stations
Table 1 Table 2 Table 3 Table 4 Table 5 Table 6
Introduction Materials and Methods Results Discussion Tables
Table 3: Comparison of the meteorological
features at two localities of years with many bluetongue outbreaks in sheep
flocks to poor bluetongue years
Years with
bluetongue epizootics (>30 flocks)
|
|
Bet Dagan | Kefar Blum |
|
Year |
75 |
87 |
88 |
94 |
Average |
75 |
87 |
88 |
94 |
Average |
|
Meteorological parameter |
||||||||||
|
Average maximum temp. of the coldest month
(Dec.-Mar) |
17.9 |
18.0 |
17.5 |
18.7 |
18.0 |
16.3 |
17.2 |
16.1 |
17.5 |
16.8 |
|
Average winter maximum temp. (Dec.-Mar.) |
19.3 |
19.0 |
18.5 |
19.9 |
19.2 |
18.2 |
18.5 |
17.5 |
19.5 |
18.4 |
|
Winter minimum temp. (Dec.-Mar.) |
1.1 |
1.9 |
2.0 |
3.5 |
2.1 |
0 |
0 |
0 |
0.6 |
0.2 |
|
Total days in Jan.-Feb. with maximum temp. of
130C and above |
56 |
58 |
57 |
59 |
58 |
54 |
55 |
50 |
57 |
54 |
|
Total days in Jan.-Feb. with maximum temp. of
180C and above |
27 |
38 |
22 |
47 |
34 |
16 |
34 |
24 |
31 |
26 |
|
*Average seasonal rainfall (mm) |
523 |
643 |
599 |
384 |
537 |
523 |
643 |
599 |
384 |
537 |
|
Total days in winter (Nov-Mar) with min. temp.
of 50C and below |
23 |
34 |
17 |
4 |
19.5 |
41 |
48 |
26 |
33 |
37 |
|
Maximum spring temperature (1 Apr-15 Jun) |
37.2 |
39.4 |
43.2 |
41.2 |
40.3 |
37.9 |
39.4 |
40.9 |
38.0 |
39 |
|
Number of Sharav days |
7 |
2 |
5 |
6 |
5 |
10 |
8 |
10 |
20 |
12 |
|
*Average rainfall in Mar-May (mm) Years with no bluetongue epizootics (0-1 flock) |
||||||||||
|
Year |
80 |
81 |
83 |
94 |
Average |
75 |
87 |
88 |
94 |
Average |
|
Average maximum temp. of the coldest month
(Dec.-Mar) |
16.8 |
16.7 |
14.9 |
18.7 |
18.0 |
16.3 |
17.2 |
16.1 |
17.5 |
16.8 |
|
Average winter maximum temp. (Dec.-Mar.) |
18.3 |
18.8 |
17.0 |
19.9 |
19.2 |
18.2 |
18.5 |
17.5 |
19.5 |
18.4 |
|
Winter minimum temp. (Dec.-Mar.) |
1.0 |
2.5 |
0.2 |
3.5 |
2.1 |
0 |
0 |
0 |
0.6 |
0.2 |
|
Total days in Jan.-Feb. with maximum temp. of
130C and above |
59 |
58 |
45 |
59 |
58 |
54 |
55 |
50 |
57 |
54 |
|
Total days in Jan.-Feb. with maximum temp. of
180C and above |
15 |
17 |
11 |
47 |
34 |
16 |
34 |
24 |
31 |
26 |
|
*Average seasonal rainfall (mm) |
728 |
608 |
686 |
384 |
537 |
523 |
643 |
599 |
384 |
537 |
|
Total days in winter (Nov-Mar) with min. temp.
of 50C and below |
28 |
24 |
42 |
4 |
19.5 |
41 |
48 |
26 |
33 |
37 |
|
Maximum spring temperature (1 Apr-15 Jun) |
42.0 |
37.2 |
36.6 |
41.2 |
40.3 |
37.9 |
39.4 |
40.9 |
38.0 |
39 |
|
Number of Sharav days |
12 |
2 |
1 |
6 |
5 |
10 |
8 |
10 |
20 |
12 |
|
*Average rainfall in Mar-May (mm) |
121 |
79 |
129 |
48 |
94 |
121 |
79 |
129 |
48 |
94 |
Table 1 Table 2 Table 3 Table 4 Table 5 Table 6
Introduction Materials and Methods Results Discussion Tables
Table 4: Numbers of Culicoides spp. suction
light trapped in the mountain and Arava areas, i.e., bluetongue free zones
versus Bet Dagan zone where bluetongue prevails
|
Locality, region (longitude and latitude) |
Altitude |
Month/year |
Location of trap: host/breeding site |
Average no. of Culicoides spp. per night/per trap |
Average no. of Culicoides spp. per
night/per trap at Bet Dagan |
|
Beit Jann, Upper Galilee |
920 |
8-10/81 ; |
goats |
<1 C. obsoletus; <1 C. imicola <1 C. circumscriptus; <1 C. schultzei gp <1 C. cataneii 1 C. obsoletus |
47 C. imicola; 6 C. schultzei gp.; 5 C. distinctipennis; 7 C. circumscriptus; <1 C. cataneii; <1 C. puncticollis; <1 C.
newsteadi; |
|
Ein Kerem (Agr. School), Judean Hills (310 46'N 350 10'E) |
660 |
9/78 |
cows |
3 C. imicola; <1 C. newsteadi <1 C. sp. |
; 131 C.
imicola; 33 C. distinctipennis; 5 C. schultzei gp; 1 C. cataneii <1 C. newsteadi; <1 C. circumscriptus |
|
Yotvata, Arava Valley (290 53'N 350 03'E) |
75 |
8/82 |
cows |
95 C. imicola; <1 C. obsoletus; <1 C. schultzei gp |
629 C. imicola; 74 C. schultzei gp; 26 C. distinctipennis;
3 C. newsteadi; <1 C. obsoletus; 1
C. circumscriptus |
|
11/82 |
cows
|
72 C. imicola; 4 C. schultzei gp.; |
10 C. imicola; 8 C. schultzei gp >1 C. distinctipennis; <1 C.
newsteadi; <1 C. obsoletus; <1 C. circumscriptus |
Table 1 Table 2 Table 3 Table 4 Table 5 Table 6
Introduction Materials and Methods Results Discussion Tables
Table 5: Average numbers per night, per trap
of Culicoides spp. suction light trapped in two
sites at Beit Dagan, Rehovot district in June, a month before the bluetongue
season
|
Bet
Dagan, Veterinary Institute Animal
compound |
Bet Dagan, Volcani Center experimental
dairy farm |
|
1982 |
1982 |
|
8 C.
obsoletus |
345 C.
imicola |
|
>3 C. imicola |
10 C.
schultzei gp |
|
<1 C. cataneii |
8 C.
circumscriptus |
|
<1 C. newsteadi |
6 C.
distinctipennis |
|
<1 C. puncticollis |
5 C.
newsteadi |
|
<1 C. circumscriptus |
2 C.
cataneii |
|
|
<1 C. obsoletus |
|
|
<1 C. puncticollis |
|
|
|
|
1996 |
1996 |
|
17 C.
imicola |
18 C.
imicola |
|
<1 C.
circumscriptus |
<1 C.
circumscriptus |
Table 1 Table 2 Table 3 Table 4 Table 5 Table 6
Introduction Materials and Methods Results Discussion Tables
Table 6: Numbers of Culicoides species
per night per trap in the winter of 1997/98
(November 1997-March 1998)
|
Month |
No. of trappings/no. of traps |
Species |
|
11/97 |
7/4 |
170 C. imicola |
|
|
|
7 C. schultzei gp. |
|
12/97 |
8/4 |
38 C. imicola |
|
|
|
1.5 C. schultzei gp. |
|
|
|
<1 C. puncticollis |
|
1/98 |
5/4 |
10 C. imicola |
|
|
|
<1 C. schultzei gp. |
|
|
|
<1 C. puncticollis |
|
2/98 |
9/4 |
6 C. imicola |
|
|
|
<1 C. schultzei gp. |
|
|
|
<1 C. circumscriptus |
|
|
|
|
|
3/98 |
9/4 |
6 C. imicola |
|
|
|
<1 C. schultzei gp. |
|
|
|
<1 C. circumscriptus |
Table 1 Table 2 Table 3 Table 4 Table 5 Table 6
Introduction Materials and Methods Results Discussion Tables