TABLE 1. Specific values of nine predictors for
each year from 1950 through 1990 used to make the 1 August forecasts of
subsequent seasonal TC activity. Data in columns 4, 5, and 8 are expressed
in terms of standardized deviations. Note that data in columns 6, 7, and
9 are departures from the long-term (1950-1990) means.
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50 mb |
30 mb |
Absolute shear |50-30 mb| |
Western sahelian (std. dev.) June-July |
Gulf of Guinea Previous yr (std. dev.) Aug-Nov. |
SLPA (mb) June-July |
ZWA (ms -1) June-July |
SOI (std. dev.) June-July |
SSTA (C) June-July |
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TABLE 2. Ratios for each of seven indexes of
TC activity for those years comprising the 10 highest yearly values versus
the 10 lowest yearly values for each of the nine predictor indices occurring
during the 41 -year period from 1950 through 1990. For example, the ratio
of HDP for the 10 most westerly QBO years to the 10 most easterly QBO years
is 2.48, as shown in the upper right of the array.
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U 50-mb QBO | |||||||
10 low / 10 high |
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U 30-mb QBO | |||||||
10 low / 10 high |
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U 50-30mb QBO-shear | |||||||
10 low / 10 high |
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Western Sahelian rain-june-July | |||||||
10 high / 10 low |
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Gulf of Guinea rain-Aug-Nov. | |||||||
10 high / 10 low |
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SLPA-June-July | |||||||
10 low / 10 high |
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ZWA-June-July | |||||||
10 low / 10 high |
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SOI-June-July | |||||||
10 high / 10 low |
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SSTA-June-July | |||||||
10 low / 10 high |
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TABLE 3. Listing of the 10 highest and the 10
lowest years for each predictor used to compute the ratios in Table
2.
Predictive Parameter | 10 high years | 10 low years |
1. Extrapolated | 1952, 54, 56, 62, 63 | 1950, 53, 55, 61, 64 |
QBO U50 | 1968, 77, 82, 84, 87 | 1969, 76, 78, 85, 88 |
2. Extrapolated | 1954, 56, 60, 65, 68 | 1950, 55, 59, 61, 69 |
QBO U30 | 1974, 77, 79, 84, 89 | 1971, 75, 80, 85, 90 |
3. Extrapolated | 1958, 60, 63, 65, 68 | 1950, 55, 57, 66, 69 |
QBO |U50-U30| | 1979, 81, 83, 86, 88 | 1971, 80, 85, 87, 90 |
4.) Western-Sahelian rain | 1952, 53, 54, 55, 60 | 1966, 72, 73, 76, 77 |
June-July | 1961, 64, 69, 75, 89 | 1980, 83, 84, 86, 87 |
5. Gulf of Guinea rain | 1950, 52, 55, 58, 61 | 1951, 59, 62, 65, 73 |
Aug-Nov. (previous year) | 1963, 64, 69, 80, 88 | 1979, 82, 83, 84, 87 |
6. Caribbean SLPA | 1968, 71, 74 75, 76 | 1951, 54, 55, 57, 58 |
June-July | 1977, 82, 85, 86, 89 | 1964, 67, 69, 83, 87 |
7. ZWA-Caribbean | 1957, 59, 65, 72, 73 | 1950, 54, 55, 58, 60 |
June-July | 1974, 76, 82, 86, 87 | 1962, 66, 69, 79, 88 |
SOI | 1950, 55, 56, 68, 73 | 1951, 63, 65, 72, 76 |
June-July | 1975, 79, 81, 88, 89 | 1977, 82, 83, 85, 87 |
9. SSTA (eastern Pacific) | 1951, 57, 65, 69, 72 | 1950, 54, 55, 64, 70 |
June-July | 1976, 80, 82, 83, 87 | 1973, 75, 84, 85, 88 |
TABLE 4. Pearson product-moment correlation coefficients
(r) for each of the seven measures of seasonal TC activity
with each of the nine seasonal predictors.
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1. QBO 50 mb | -0.46 | -0.54 | -0.41 | -0.46 | -0.48 | -0.36 | -0.45 |
2. QBO 30 mb | -0.51 | -0.57 | -0.54 | -0.53 | -0.50 | -0.36 | -0.49 |
3. shear | -0.20 | -0.21 | -0.29 | -0.24 | -0.18 | -0.12 | -0.19 |
4. Western Sahelian | 0.39 | 0.53 | 0.39 | 0.52 | 0.64 | 0.71 | 0.60 |
5. Gulf of Guinea | 0.51 | 0.60 | 0.57 | 0.59 | 0.67 | 0.63 | 0.63 |
6. SLPA | -0.33 | -0.38 | -0.31 | -0.39 | -0.41 | -0.37 | -0.40 |
7. ZWA | -0.38 | -0.33 | -0.35 | -0.40 | -0.45 | -0.45 | -0.44 |
8. SOI | 0.29 | 0.38 | 0.31 | 0.33 | 0.36 | 0.30 | 0.35 |
9. SSTA | -0.34 | -0.19 | -0.20 | -0.18 | -0.22 | -0.21 | -0.19 |
TABLE 5. Empirical weights for composite functions
of QBO, African rainfall, and Caribbean basin-ENSO data for the jackknifed
LAD regression procedure prediction equations.
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NS | 1,000 | 0.711 | -0.082 | 1,000 | -1.260 | 1,000 | 0.106 | -0.275 | 0.046 |
NSD | 1,000 | 0.560 | -0.358 | 1,000 | 1.109 | 1,000 | 0.096 | -0.864 | -1.489 |
H | 1,000 | 1.928 | 0.284 | 1,000 | 17.876 | 1,000 | -1.172 | -1.966 | -0.025 |
HD | 1,000 | 0.894 | 0.266 | 1,000 | 0.613 | 1,000 | 0.182 | 0.050 | -0.075 |
IH | 1,000 | 0.614 | -0.467 | 1,000 | 0.591 | 1,000 | 0.051 | 0.474 | 0.630 |
IHD | 1,000 | 0.730 | 2.777 | 1,000 | 0.248 | 1,000 | -0.019 | 1.272 | 0.567 |
HDP | 1,000 | 0.608 | 0.629 | 1,000 | 0.256 | 1,000 | 0.169 | 0.705 | 0.312 |
TABLE 6. Agreement coefficient ,
probability P, and r2 values from a jackknifed
LAD regression procedure.
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NS | 0.447 | 0.33 x 10-6 | 0.433 |
NSD | 0.608 | 0.14 x 10-8 | 0.584 |
H | 0.472 | 0.48 x 10-6 | 0.455 |
HD | 0.505 | 0.23 x 10-6 | 0.558 |
IH | 0.618 | 0.25 x 10-8 | 0.677 |
IHD | 0.617 | 0.50 x 10-9 | 0.598 |
HDP | 0.556 | 0.12 x 10-7 | 0.584 |
TABLE 7. Measures of agreement p between observed
and predicted values associated with nonjackknifed and both grouped (G)
and nongrouped (NG) jackknifed LAD and OLS regression procedures.
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LAD regression model: | |||||||
1 December forecast results | |||||||
Nonjackknifed | .440 | .514 | .447 | .493 | .498 | .451 | .457 |
Jackknified-G | .440 | .514 | .447 | .491 | .498 | .451 | .447 |
Jackknified-NG | .411 | .386 | .279 | .305 | .376 | .374 | .235 |
1 August forecast results | |||||||
Nonjackknifed | .447 | .608 | .472 | .516 | .618 | .617 | .557 |
Jackknified-G | .447 | .608 | .472 | .505 | .618 | .617 | .556 |
Jackknified-NG | .186 | .435 | .256 | .210 | .544 | .499 | .325 |
OLS regression model: | |||||||
1 December forecast results | |||||||
Nonjackknifed | .359 | .407 | .388 | .400 | .491 | .450 | .430 |
Jackknified-G | .308 | .359 | .339 | .355 | .448 | .403 | .385 |
Jackknified-NG | .244 | .306 | .280 | .300 | .408 | .367 | .338 |
1 August forecast results | |||||||
Nonjackknifed | .435 | .528 | .428 | .489 | .605 | .579 | .531 |
Jackknified-G | .374 | .477 | .367 | .432 | .562 | .529 | .476 |
Jackknified-NG | .270 | .388 | .247 | .330 | .490 | .450 | .379 |
TABLE 8. Squared Pearson product-moment correlation
coefficients r2 between observed and predicted values associated
with nonjackknifed and both grouped (G) and nongrouped (NG) jackknifed
LAD and OLS regression procedures.
NS | NSD | H | HD | IH | IHD | HDP | |
LAD regression model: | |||||||
1 December forecast results | |||||||
Nonjackknifed | .395 | .488 | .466 | .514 | .581 | .517 | .544 |
Jackknified-G | .395 | .488 | .466 | .511 | .581 | .517 | .527 |
Jackknified-NG | .368 | .358 | .280 | .320 | .415 | .431 | .276 |
1 August forecast results | |||||||
Nonjackknifed | .433 | .584 | .455 | .573 | .677 | .598 | .585 |
Jackknified-G | .433 | .584 | .455 | .558 | .677 | .598 | .584 |
Jackknified-NG | .164 | .436 | .198 | .198 | .593 | .509 | .302 |
OLS regression model: | |||||||
1 December forecast results | |||||||
Nonjackknifed | .416 | .523 | .482 | .538 | .585 | .545 | .570 |
.Jackknified-G | .313 | .434 | .391 | .464 | .502 | .454 | .495 |
Jackknified-NG | .202 | .347 | .299 | .378 | .433 | .399 | .423 |
1 August forecast results | |||||||
Nonjackknifed | .527 | .649 | .511 | .597 | .711 | .668 | .643 |
Jackknified-G | .406 | .564 | .399 | .504 | .646 | .577 | .556 |
Jackknified-NG | .255 | .430 | .154 | .321 | .528 | .449 | .394 |
TABLE 9. Regression weights for the nonjackknifed
(LAD) regression procedure prediction equations.
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