To better understand the controls on the opportunistic human pathogen
Vibrio vulnificus
in warm tropical waters, we conducted a year-long investigation in the Ala Wai Canal, a channelized estuary in Honolulu, HI. The abundance of
V. vulnificus
as determined by qPCR of the hemolysin gene (
vvhA
), varied spatially and temporally nearly four orders of magnitude (≤ 3 to 14,000 mL
−1
). Unlike in temperate and subtropical systems, temperatures were persistently warm (19–31°C) and explained little of the variability in
V. vulnificus
abundance. Salinity (1–36 ppt) had a significant, but non-linear, relationship with
V. vulnificus
abundance with highest
vvhA
concentrations (> 2,500 mL
−1
) observed only at salinities from 7 to 22 ppt.
V. vulnificus
abundances were lower on average in the summer dry season when waters were warmer but more saline. Highest canal-wide average abundances were observed during a time of modest rainfall when moderate salinities and elevated concentrations of reduced nitrogen species and silica suggested a groundwater influence. Distinguishing the abundances of two genotypes of
V. vulnificus
(C-type and E-type) suggest that C-type strains, which are responsible for most human infections, were usually less abundant (25% on average), but their relative contribution was greater at higher salinities, suggesting a broader salinity tolerance. Generalized regression models suggested up to 67% of sample-to-sample variation in log-transformed
V. vulnificus
abundance was explained (n = 202) using the measured environmental variables, and up to 97% of the monthly variation in canal-wide average concentrations (n = 13) was explained with the best subset of four variables.
IMPORTANCE
Our data illustrate that, in the absence of strong seasonal variation in water temperature in the tropics, variation in salinity driven by rainfall becomes a primary controlling variable on
V. vulnificus
abundance. There is thus a tendency for a rainfall-driven seasonal cycle in
V. vulnificus
abundance that is inverted from the temperature-driven seasonal cycle at higher latitudes. However, stochasticity in rainfall and its non-linear, indirect effects on
V. vulnificus
concentration means that high abundances can occur at any location in the canal at any time of year, making it challenging to predict concentrations of this pathogen at high temporal or spatial resolution. Much of the variability in canal-wide average concentrations, on the other hand, was explained by a few variables that reflect the magnitude of freshwater input to the system, suggesting that relative risk of exposure to this pathogen could be predicted as an average for the system.