et al., 2007). In addition to the significant burden of seasonal
influenza, the persistent threat is that a pandemic causing strain
may appear due to antigenic shift or reassortment.
There are three types of influenza virus circulating in the world:
A, B and C. Type A and B are the most commonly found in
humans. Type A is further classified into subtypes (e.g., HIN1)
based on the types of hemagglutinin and neuraminidase on the
surface of the virus.
In order to accommodate the ever changing circulating
influenza strain, vaccine composition recommendations are
updated twice a year. The recommendations are made by the
World Health Organization (WHO) through its Global
Influenza Surveillance Network (GISN).
2. ENVIRONMENTAL DETERMINANTS
2.1 Malaria and Dengue
Many factors are known to contribute to malaria transmission,
including meteorological and environmental conditions,
socioeconomic status, military conflicts and natural disasters.
Among these, meteorological and environmental factors are
perhaps the most noticeable. For example, malaria transmission
may increase with the arrival or the end of a rainy season, and
living near forest or water bodies may pose greater risk of
mosquito bites and getting malaria. The El Nifio-Southern
Oscillation (ENSO) is a quasi-periodic climatic cycle that
occurs every three to seven years across the tropical Pacific
Ocean, and which causes excessive precipitation or droughts,
has been shown to promote malaria transmission (Kovats 2003).
Aside from precipitation, temperature and humidity are also
important factors. Warmer temperatures hasten larval and
vector development, and prolong mosquito life span and its
consequent ability to transmit malaria. Warmer air retains more
moisture and improves mosquito survivorship, so is higher
humidity.
Vegetation has also been linked to malaria as it indicates the
vector’s breeding sites. For example, Anopheles dirus is a forest
breeder, and An. maculates and An. sawadwongpori are rice
field breeders. The Normalized Difference Vegetation Index
(NDVI) (Tucker 1979) is one of the indices for vegetation
condition. It is defined as the difference between the responses
from the infrared and the red bands normalized by their mean.
In modelling infectious diseases, NDVI is used most often to
infer the precipitation which the area received before the
satellite measurements were taken. The spatial distribution of
NDVI can also be used to differentiate among urban, peri-
urban, suburban and rural areas. Such information on the nature
of the area is useful for malaria prevention and control.
Like malaria, temperature, humidity and rainfall are the
important environmental determinants for dengue transmission.
However, their effects on dengue transmission may be less
obvious than those for malaria transmission because dengue
vectors can breed indoor.
2.2 Influenza
The spatiotemporal variation of influenza across latitudes
suggests that climate and environmental factors may have roles
in influenza transmission and pathogenesis.
It is well known that influenza transmission in temperate
climates is seasonal and peaks in the winter months. In the US,
for example, influenza outbreaks often start as early as October,
peak in February, and diminish by April or May; thus forming a
distinct inter-annual oscillation pattern. In the tropics, there are
significant influenza cases throughout the year, with one or two
less distinct peak(s) whose timing varies geographically. It has
been shown (e.g., Viboud et al., 2006) that influenza seasonal
patterns vary with latitude, forming a traveling wave across the
globe. Several studies that have explored the global migration
pattern of influenza show varying travel pattern of influenza
virus A migration out of the tropics and China; and migration
between northern and southern hemispheres. Another study in
Brazil showed that influenza starts in a low-population state
near the equator during March-April, and travels southward
towards temperate and more populous states (Alonso et al.,
2007). Temperature, humidity and rainfall are among the
factors that have been frequently implicated in influenza
transmission.
3. REMOTE SENSING MEASUREMENTS
Satellite measurements of precipitation for estimating disease
risks are most often derived from the Tropical Rainfall
Monitoring Mission (TRMM) (Kummerow 1998). TRMM is a
collaboration between the US and Japan. Japan built the
precipitation radar (PR) and launched the spacecraft in 1999.
There are five instruments on board: PR, TRMM microwave
imager (TMI), Visible and Infrared Scanner (VIIRS), Cloud and
Earth Radiation Energy Sensor (CERES), and Lighting Image
Scanner (LIS). The main sensor that measures precipitation is
TMI. Because the spatial resolution of the TRMM measurement
is low, sometimes NDVI measured from a medium resolution
satellite is used to infer the recent rainfall at a higher spatial
resolution. Such inference is most effective for arid regions
where little rainfall is received and vegetation growth is
sensitive to rainfall, but less effective for regions with plenty
rainfall. Land surface temperature and NDVI are both provided
by the moderate resolution imaging spectroradiometer
(MODIS). This sensor has thirty-six bands spanning the visible
to the near-infrared wavelengths. Both the Terra and Aqua
observatories are equipped with MODIS. NDVI, however, can
be computed from any satellite instruments with red and
infrared channels. However, because of the differences in band
definitions, instrument characteristics, satellite orbits and
measuring conditions, NDVI from different sensors must first
be cross calibrated before they can be compared. In addition to
the datasets described above, quite a few other satellites also
provide data for ground cover classification, identification of
potential larval habitats, and modelling malaria risks. For
example, the well-known Landsat and SPOT series of satellites
and the Advanced Spaceborne Thermal Emission and
Reflection Radiometer (ASTER) and the Advanced Land
Imager (ALI) (USGS 2009) are some of the multispectral
sensors used for health monitoring purposes. Microwave
sensors like Radarsat and the Phased Array L-band Synthetic
Aperture Radar (PALSAR) are used over areas that are
obscured frequently by clouds (JAXA 2011). The geoscience
laser altimeter system (GLAS) is a light detection and ranging
(LIDAR) sensor that is useful for differentiating vegetation
types (NASA 2011). For high spatial resolution imagery,
commercial data from IKONOS, QuickBird, or WorldView can
be used (GeoEye 2011; DigitalGlobe 2011).
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