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Number 101, February 2009
The Island
 
Climate Update
Collaborators
Pacific Islands National 
Meteorological Services
Australian Bureau of 
Meteorology
Meteo France
NOAA National 
Weather Service
NOAA Climate 
Prediction Centre 
(CPC)
International Research 
Institute for Climate 
and Society
European Centre 
for Medium Range 
Weather Forecasts
UK Met Office
World Meteorological 
Organization
MetService of
New Zealand
January’s climate
  The South Pacific Convergence Zone (SPCZ) was displaced 
southwest of its normal position and was very active.  
  Very suppressed convection near Western Kiribati and south of the 
Equator from Nauru east to northern French Polynesia. 
  Normal to well above normal rainfall for many areas in the South 
Pacific, with many new records established in Fiji.
El Niño/Southern Oscillation (ENSO), seasonal 
rainfall, and sea surface temperature forecasts
  La Niña-like conditions exist in the tropical Pacific. Many climate 
models project continuation of La Niña through to the end of 
summer 2009.
  Below normal rainfall is forecast for Western Kiribati, Tuvalu, 
Tokelau, the Northern Cook Islands, and the Society Islands.
  Above normal rainfall is expected for New Caledonia, Niue, Tonga, 
and Papua New Guinea.
  Normal to above normal SSTs are forecast for the southwestern half 
of the southwest Pacific region. Normal to below normal SSTs are 
forecast for the northeast half of the southwest Pacific.   
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The Island Climate Update, No. 101, February 2009
Page 2
Climate developments in January 2009
Outgoing Long-wave Radiation (OLR) anomalies, in Wm
2
 are represented 
by  hatched  areas.  High  radiation  levels  (yellow)  are  typically  associated 
with  clearer  skies  and  lower  rainfall,  while  cloudy  conditions  lower  the 
OLR (blue) and typically result in higher rainfall. The January 2009 position 
of the South Pacific Convergence Zone (SPCZ) was displaced southwest of 
its normal position, and much more coherent than last month.  The average 
position of the SPCZ is identified by the dashed green line, which is based 
on mean January rainfall for the South Pacific. Mean sea level (MSL) pressure 
anomalies (in hPa) are shown as grey lines.
-90 -70 -50 -30 -20 -10 10 20 30 50 70 90
Australia
NewZealand
Fiji
NewCaledonia
Vanuatu
SolomonIs
Pitcairn
Samoa
Tonga
Niue
E Kiribati
Papua NewGuinea
NCook Is
S Cook Is
Society Is
WKiribati
Line Is
Tuvalu
Marquesas Is
Austral Is
Marshall Is
Rawaki Is
TokelauIs
Nauru
Fed States of Micronesia
Tuamotu Is
EQUATOR
Wallis & Futuna
H
H
H
H
Soil moisture in January 2009
Estimated  soil  moisture  conditions  at  the  end  of  January  2009, 
using monthly rainfall data. Soil moisture projections for individual 
Pacific  Island  countries  are  dependent  on  data  availability  at  the 
time of publication.
E
stimates  of  soil  moisture  shown  in  the  map  (right)  are 
based on monthly rainfall for one station in each country.  
Currently there are not many sites in the water balance model, 
but more stations will be included in the future. 
The information displayed is based on a simple water balance 
technique  to  determine  soil  moisture  levels.  Addition  of 
moisture  to  the  available  water  already  in  the  soil  comes 
from  rainfall,  with  losses  via  evapotranspiration.  Monthly 
rainfall  and  evapotranspiration  are  used  to  determine  the 
soil  moisture  level  and  its  changes.  These  soil  moisture 
calculations  were  made  at  the  end  of  the  month,  and  for 
practical  purposes,  generalisations  were  made  about  the 
available water capacity of the soils at each site. 
Nadi  (Fiji),  Hanan  (Niue),  Port  Vila  (Vanuatu),  Rarotonga 
(Southern  Cook  Islands),  and  Apia  (Samoa)  project  moist 
(at or near field capacity) soil moisture conditions. Soils are 
moderate for the time of year at Nuku’alofa (Tonga).
T
he South Pacific Convergence Zone (SPCZ) activity was 
displaced  south  and  west  of  normal  during  January, 
and  was  more  consolidated  than  last  month.  A  region  of 
enhanced rainfall due to intensified convection was observed 
during  January  2009  over  northeast  Australia,  and  in  the 
south Pacific extending from the Solomon Islands southeast 
to the Southern Cook Islands. Very high amounts of rainfall 
occurred within this band, and are highlighted in this issue. 
Suppressed  convection  intensified  during  the  month  near 
the  Equator,  and  encompassed  the  region  northeast  of  the 
Solomon Islands that included Nauru and Western Kiribati, 
and extended across the southwest Pacific to the Marquesas. 
The regional circulation for the month was characterised by 
more  frequent  high  pressure  across  the  northeastern  half 
of the South Pacific; and lower than normal pressures east 
of northern New Zealand and south of the Southern Cook 
Islands. 
Many rainfall records were shattered in Fiji in January 2009 
(see back page highlight article), with most stations receiving 
140–450%  of  normal  rainfall.  Similarly,  northeastern 
Australia  (220–250%  or  normal),  Vanuatu  (135–200%  of 
normal),  and  Tonga  (120–340%  of  normal)  received  well 
above normal rainfall for many stations.  Enhanced rainfall 
was also localised near Pitcairn Island. All of the reporting 
stations  for  Tonga  received  greater  than  300mm  rainfall  in 
January, and two of those stations were close to or exceeded 
previous monthly record highs.
Lower than normal rainfall was recorded at many stations in 
French Polynesia, with Hiva Hoa in the Marquesas Islands 
receiving 34 mm of rainfall (22% of normal). Elsewhere in 
the eastern half of the southwest Pacific, the stations in the 
Tuamotu  archipelago  and  the  Austral  Islands  all  recorded 
normal  or  below  normal  rainfall,  except  Rikitea,  which 
received a record high total of 433 mm (297% of normal).
Continuing the trend from last month, many stations in New 
Caledonia  received  well  below  normal  rainfall  (30–60%) 
during January. Northern New Zealand also experienced a 
relatively dry month, with the northern part of the country 
recording  well  below  normal  rainfall  (20–60%  of  normal). 
The  Solomon  Islands  also  had  a  relatively  normal  month, 
except  at  Honiara  and  Henderson,  which  received  170–
Wet
Moderate
Dry
Wet
Moderate
Dry
Wet
Moderate
Dry
Wet
Moderate
Dry
January 2009 
January 2008
Island Group
Location
Rainfall
(mm)
% of 
avg
Comments
Fiji
Lautoka
1291
348
Record high; 
Highest monthly 
total in the region
Tonga
Fua’amotu
570
284
Record high
Fiji
Penang
1228
310
Record high
Tuamotu
Rikitea
433
297
Record high
Marquesas
Hiva Hoa
34
22
Very low
New Caledonia
Belep
60
25
Very low
190% of normal rainfall.
 
Australia
 
New Zealand
 
Fiji
 
New Caledonia
 
Vanuatu
 
Solomon Is
 
Samoa
 
Tonga
 
Niue
 
E Kiribati
 
Papua New Guinea
 
S Cook Is
 
N Cook Is
 
Society Is
 
W Kiribati
 
Line Is
 
Tuvalu
 
Marquesas Is
 
Austral Is
 
Marshall Is
 
Rawaki Is
 
Tokelau Is
 
Nauru
 
Tuamotu Is
 
Pitcairn
 
EQUATOR
 
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The Island Climate Update, No. 101, February 2009
Page 3
Mean sea surface temperatures (ºC) for January 2009 
Sea surface temperature anomalies (ºC) for January 2009
Forecast validation: November 2008 to January 2009
-3
-2
-1
0.5
2
3
Australia
New Zealand
Fiji
New Caledonia
Vanuatu
Solomon Is
Samoa
Tonga
Niue
E Kiribati
Papua New Guinea
S Cook Is
N Cook Is
Society Is
W Kiribati
Line Is
Tuvalu
Marquesas Is
Austral Is
Marshall Is
Rawaki Is
Tokelau Is
Nauru
Fed States of Micronesia
Tuamotu Is
Pitcairn
EQUATOR
Wallis & Futuna
10 12 14 16 18 20 22 24 26 28 30 32
Australia
New Zealand
Fiji
New Caledonia
Vanuatu
Solomon Is
Samoa
Tonga
Niue
E Kiribati
Papua New Guinea
S Cook Is
N Cook Is
Society Is
W Kiribati
Line Is
Tuvalu
Marquesas Is
Austral Is
Marshall Is
Rawaki Is
Tokelau Is
Nauru
Fed States of Micronesia
Tuamotu Is
Pitcairn
EQUATOR
Wallis & Futuna
El Niño/Southern Oscillation (ENSO)
D
uring  January,  La  Niña  conditions  were 
established in the equatorial Pacific Ocean, with 
the tropical Pacific atmosphere exhibiting moderate 
La Niña characteristics.  The SOI remained positive 
with  a  January  value  of  +0.9  (NDJ  mean  +1.3),.
The  easterly  trade  winds  remained  strong  during 
December  about  and  west  of  the  Date  Line,  now 
have weaken slightly across the tropical Pacific, but 
still appear to strongest around 160°E. 
SST  anomalies  in  December  were  below  average 
across the Equatorial Pacific: the NINO3 anomaly for 
strengthened  in  January  to  –0.7°C  (3-month  mean 
–0.3°C), as did the NINO4 anomaly which is –0.7°C 
(OND mean  0.4°C). Equatorial subsurface anomalies 
that  strengthened  at  the  thermocline  in  December 
(with a –4°C anomaly centred near 140°W below 
100m) now appear to be weakening somewhat in the 
eastern equatorial Pacific with some weak warming 
at  the  surface  near  South  American  Coast.    West 
of  the  dateline  sub-surface  warming  appears  to  be 
occurring and intensifying towards 160°W.
Tropical  Pacific  precipitation  patterns  continue  to 
exhibit La Niña characteristics, with the TRMM ENSO 
precipitation  index  at  -0.82  for  January  (up  from 
-1.34 in December). OLR anomalies show extremely 
suppressed  equatorial  convection  about  and  west 
of the Date Line and the eastern Indian Ocean for 
January as a whole, with enhanced convection over 
the maritime continent and northern Australia. The 
MJO in the Indian Ocean is weak and is expected to 
remain so into the second week of February.
Several  climate  models  assessed  by  NIWA  predict 
weakening La Niña conditions over the next three-
months (FMA). The majority indicate ENSO-neutral 
conditions  during  late  autumn  and  early  winter 
2009.  The  NCEP  discussion  of  8  January  indicates 
a  continuation  of  below  average  sea  surface 
temperatures  and  continuation  of  La  Niña  through 
early 2009. The IRI summary of 14 January indicates 
A
 
 
 
region  of  suppressed  convection  was  expected  to 
encompass the central and eastern Southwest Pacific, in 
a region extending from Western Kiribati to the Marquesas 
Islands  and  the  Society  Islands,  including  Tuvalu,  Tokelau, 
Wallis  &  Futuna,  Samoa,  the  Northern  Cook  Islands,  and 
the Tuamotu archipelago. Below normal or near–to–below 
normal rainfall was expected for those countries. Enhanced 
convection  was  expected  to  be  focused  near  Papua  New 
Guinea,  and  also  near  Vanuatu,  New  Caledonia,  Tonga, 
Fiji,  and  Niue  with  above  average  rainfall.  Near–to–above 
average rainfall was forecast for the Southern Cook Islands, 
the  Austral  Islands,  and  Pitcairn  Island,  while  no  clear 
precipitation forecast was offered for the Solomon Islands. 
The rainfall outlook for the November 2008–January 2009 
period was calculated for 17 island groups (one island had 
a forecast of ‘climatology’, which is unscoreable, and three 
did not report values). The global station ‘hit’ rate was 71%, 
7% higher than average for forecasts made during November 
and 10% higher than the average for all months combined. 
Rainfall was overprojected for Vanuatu and New Caledonia, 
and  either  over–  or  under–  projected  for  parts  of  French 
Polynesia.
a  55%  chance  of  La  Niña  conditions  persisting  over  the 
coming season, and 45 – 50 % chance of a return to ENSO-
neutral conditions. 
Tropical Cyclone Activity and Guidance
T
ropical cyclone Hettie, the first to form in the southwest Pacific during the 2008–09 season, developed on 28th January to 
the southeast of Fiji. The system brought southerly winds and heavy rain to the central region of Fiji on the 28–29 January, 
and then tracked to the southwest before dissapating on 30 January. Conditions in the tropical Pacific are still likely to affect 
the chances of tropical cyclone (TC) activity for several countries between January and May 2009. There is an increased risk 
of TC occurrence for countries west of the Date Line, including Vanuatu, the Solomon Islands, and New Zealand, and a slight 
risk increase for New Caledonia. Reduced risk is expected for Samoa, Tonga, and Niue.
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The Island Climate Update, No. 101, February 2009
Page 4
Tropical Pacific rainfall – January 2009
Rainfall totalling 200% or more is considered well above average. Totals of 40% or less are normally well below average. Highlighted values are 
new records. 
Data are published as received and may be subject to change after undergoing quality control checks. N/A denotes data unavailability at the time 
of publishing, and * denotes synoptic values.
Territory and 
station station 
name
January 2009 
rainfall 
total (mm)
January 2009 
percent of
average
Australia
Cairns Airport
882
223
Townsville Airport
664
245
Brisbane Airport
77
49
Sydney Airport
25
25
Cook Islands
Penrhyn
28
11
Aitutaki
221
86
Rarotonga Airport
137
61
Fiji
Rotuma Island
500
141
Udu Point
700
224
Nadi Airport
1181
344
Nausori
652
179
French Polynesia
Hiva Hoa, Atuona
34
22
Bora Bora
201
81
Tahiti – Faa’a
261
96
Tuamotu, Takaroa
123
64
Gambier, Rikitea
433
297
Tubuai
67
33
Rapa
110
46
Kiribati
Tarawa
 N/A
N/A
Kanton
 N/A
N/A
New Zealand
Kaitaia
20
12
Whangarei Airport
12
14
Auckland Airport
32
48
New Caledonia
Ile Art, Belep
60
25
Koumac
96
54
Ouloup
72
41
Ouanaham
85
43
Poindimie
235
63
La Roche
215
122
La Tontouta
77
64
Noumea
75
65
Moue
150
81
Territory and 
station station 
name
January 2009 
rainfall 
total (mm)
January 2009 
percent of
average
Niue
Hanan Airport
388
114
Liku
255
103
North Tasman
Lord Howe Island
46
40
Norfolk Island
64
70
Raoul Island
19
15
Samoa
Faleolo Airport
302
123
Apia
386
79
Nafanua
607
123
Afiamalu
955
120
Maota
207
50
Solomon Islands
Taro
240
100
Munda
401
104
Auki
435
121
Honiara
509
187
Henderson
406
171
Kira Kira
377
110
Santa Cruz, Lata
491
117
Tonga
Niuafo’ou
N/A
N/A
Mata’aho Airport
326
118
Lupepau’u
392
136
Salote Airport
559
341
Nuku’alofa
346
199
Fua’amotu Airport
570
284
Tuvalu
Nanumea
4
1
Nui Island
96
23
Funafuti
445
115
Nuilakita
337.0
90
Vanuatu
Sola
557
141
Pekoa
539
166
Lamap
340
135
Port Vila
420
152
Tanna/Whitegrass
79
N/A
Aneityum
183
66
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The Island Climate Update, No. 101, February 2009
Page 5
Rainfall outlook map for February to April 2009
Tropical rainfall and SST outlook: February to April 2009
NOTE: Rainfall and sea surface termperature estimates for Pacific Islands for the next three months are given in the tables below.  The tercile probabilities (e.g., 
20:30:50) are derived from the averages of several global climate models. They correspond to the odds of the observed rainfall or sea surface temperatures being in 
the lowest one third of the distribution, the middle one third, or the highest one third of the distribution. For the long term average, it is equally likely (33% chance) 
that conditions in any of the three terciles will occur. *If conditions are climatology, we expect an equal chance of the rainfall being in any tercile.  
D
uring  the  February–April  2009  forecast  period,  a 
region of suppressed convection is likely to encompass 
the  central  and  eastern  Southwest  Pacific,  extending  to 
the southeast from Western Kiribati and including Tuvalu, 
Tokelau, the Northern Cook Islands, and the Society Islands, 
where  below  normal  rainfall  is  expected.  Near–to–below 
normal rainfall is expected for Samoa, Eastern Kiribati, the  
Tuamotu archipelago, and the Marquesas Islands.
Enhanced convection is expected to extend southeast from, 
Papua  New  Guinea,  and  includes  New  Caledonia,  Tonga 
and Niue, where above normal rainfall is forecast. Near or 
above normal rainfall is forecast for the Austral Islands, Fiji, 
the  Southern  Cook  Islands,  and  Pitcairn  Island.  No  clear 
precipitation guidance is offered for the Solomon Islands or 
Wallis & Futuna for the three-month forecast period. 
SSTs  are  expected  to  be  above  normal  around  eastern 
Papua  New  Guinea,  and  surrounding  Vanuatu,  Fiji  and 
New Caledonia. Near normal or above normal SSTs are also 
expected  for  Niue,  Tonga,  Wallis  &  Futuna,  the  Southern 
Cook  Islands,    the  Society  Islands,  Austral  Islands,  and 
Pitcairn  Island.  Near  normal  or  below  normal  SSTs  are 
forecast  for  the  Tuamotu  archipelago,  the  Northern  Cook 
Islands, Tuvalu, Tokelau, and Eastern & Western Kiribati.
The confidence in the forecast model skill for this seasonal 
rainfall  outlook  is  moderately  high  for  most  Pacific  Island 
countries. In the past, the average region-wide hit rate for 
forecasts issued in February is 63%, 1% lower than the long-
term  average  for  all  months  combined.  The  SST  forecast 
confidence is moderate–to–high for this period.
Island Group
Rainfall Outlook
Outlook confidence
New Caledonia
20:30:50 (Above)
High
Niue
20:35:45 (Above)
Moderate-High
Papua New Guinea
20:35:45 (Above)
Moderate-High
Tonga
20:35:45 (Above)
Moderate-High
Austral Islands
25:35:40 (Near or Above)
Moderate-High
Cook Islands (Southern) 
25:35:40 (Near or Above)
Moderate-High
Fiji
25:35:40 (Near or Above)
Moderate-High
Pitcairn Island
25:35:40 (Near or Above)
Moderate-High
Vanuatu
25:35:40 (Near or Above)
Moderate-High
Solomon Islands
30:35:35 (Climatology)
Moderate-High
Wallis & Futuna
30:35:35 (Climatology)
Moderate
Marquesas
35:40:25 (Near or Below)
Moderate-High
Kiribati (Eastern)
40:35:25 (Near or Below)
Moderate-High
Samoa
40:35:25 (Near or Below)
Moderate-High
Tuamotu Islands
40:35:25 (Near or Below)
Moderate-High
Cook Islands (Northern) 
45:35:20 (Below)
Moderate-High
Society Islands
45:35:20 (Below)
Moderate-High
Kiribati (Western)
50:30:20 (Below)
Moderate-High
Tokelau
50:30:20 (Below)
Moderate-High
Tuvalu
50:30:20 (Below)
Moderate-High
Australia
New Zealand
Fiji
New Caledonia
Vanuatu
Solomon Is
Pitcairn
Samoa
Tonga
Niue
E Kiribati
Papua New Guinea
N Cook Is
S Cook Is
Society Is
W Kiribati
Line Is
Tuvalu
Marquesas Is
Austral Is
Marshall Is
Rawaki Is
Tokelau Is
Nauru
Fed States of Micronesia
Tuamotu Is
EQUATOR
Wallis & Futuna
SST outlook map for February to April 2009
Island Group
SST Outlook
Outlook confidence
Fiji
20:35:45 (Above)
Moderate-High
New Caledonia
20:35:45 (Above)
Moderate-High
Papua New Guinea
20:35:45 (Above)
Moderate-High
Vanuatu
20:35:45 (Above)
Moderate-High
Austral Islands
25:35:40 (Near or above)
Moderate
Cook Islands (Southern) 
25:35:40 (Near or above)
Moderate
Niue
25:35:40 (Near or above)
Moderate-High
Pitcairn Island
25:35:40 (Near or above)
Moderate
Society Islands
25:35:40 (Near or above)
Moderate-High
Tonga
25:35:40 (Near or above)
Moderate-High
Wallis & Futuna
25:35:40 (Near or above)
Moderate-High
Samoa
25:40:35 (Near or above)
Moderate
Marquesas
30:40:30 (Near Normal)
Moderate
Solomon Islands
30:40:30 (Near Normal)
Moderate
Tuvalu
35:35:30 (Climatology)
Moderate-High
Cook Islands (Northern) 
35:40:25 (Near or Below)
Moderate-High
Tokelau
35:40:25 (Near or Below)
Moderate-High
Tuamotu Islands
35:40:25 (Near or Below)
Moderate
Kiribati (Eastern)
40:35:25 (Near or Below)
Moderate-High
Kiribati (Western)
40:35:25 (Near or Below)
Moderate-High
Australia
NewZealand
Fiji
NewCaledonia
Vanuatu
Solomon Is
Pitcairn
Samoa
Tonga
Niue
E Kiribati
Papua NewGuinea
NCook Is
S Cook Is
Society Is
WKiribati
Line Is
Tuvalu
Marquesas Is
Austral Is
Marshall Is
Rawaki Is
Tokelau Is
Nauru
Fed States of Micronesia
Tuamotu Is
EQUATOR
Wallis &Futuna
Near
Normal
Below normal
Near or below
Near or above
Above normal
background image
The Island Climate Update, No. 101, February 2009
Page 6
Acknowledgements
This  bulletin  is  produced  by  NIWA  and  made  possible 
with  financial  support  from  the  New  Zealand  Agency 
for  International  Development  (NZAID),  with  additional 
support  from  the  Pacific  Islands  Applied  Geosciences 
Commission  (SOPAC)  and  the  Secretariat  for  the 
Pacific  Regional  Environmental  Programme  (SPREP).
This summary is prepared as soon as possible following the 
end of the month, once the data and information are received 
from  the  Pacific  Island  National  Meteorological  Services 
(NMHS).  Delays  in  data  collection  and  communication 
occasionally  arise.  While  every  effort  is  made  to  verify 
observational data, NIWA does not guarantee the accuracy 
and  reliability  of  the  analysis  and  forecast  information 
presented,  and  accepts  no  liability  for  any  losses 
incurred through the use of this bulletin and its content.
The contents of The Island Climate Update may be freely 
disseminated,  provided  the  source  is  acknowledged. 
Requests for Pacific Island climate data should be directed 
to the Meteorological Services concerned.
Cover Photo: 
Wendy St George, 
NIWA
Visit The Island Climate Update at:
www.niwascience.co.nz/ncc/icu
Your comments and ideas about The Island Climate 
Update are welcome. Please contact:
Dr Andrew Lorrey, NIWA, 
41 Market Place, Auckland, New Zealand 
E-mail: 
a.lorrey@niwa.co.nz 
Forecasts: 
Dr. Andrew Lorrey (South Pacific rainfall and SST forecasts) and 
the NIWA National Climate Centre (ENSO)
ICU Editors:
Andrew Lorrey Email: 
a.lorrey@niwa.co.nz
Jim Salinger Email: 
j.salinger@niwa.co.nz
Harriet Palmer Email: 
h.palmer@niwa.co.nz
Sources of South Pacific rainfall data
This  bulletin  is  a  multi-national  project,  with  important 
collaboration  from  the  following  Meteorological  Services:
American  Samoa,  Australia,  Cook  Islands,  Fiji,  French 
Polynesia, Kiribati, New  Caledonia, New  Zealand,  Niue, 
Papua  New  Guinea,  Pitcairn  Island,  Samoa,  Solomon 
Islands,  Tokelau,  Tonga,  Tuvalu,  Vanuatu,  Wallis  and 
Futuna.
Extreme rainfall and new records in the Fiji Islands, January 2009
Fiji Meteorological Service
J
anuary 2009 was the wettest first month of the year in more than 
a century at several locations in Fiji. The total monthly rainfall 
was equivalent to or above 200% of normal at more than 75% of 
reporting stations in the Western, Central and Eastern Divisions 
of  the  country.  Fourteen  monthly  rainfall  totals  and  seven 
24hr daily rainfall records were broken during the month. The 
considerable amount of rainfall was due to a number of intense 
synoptic  scale  weather  features  that  impacted  the  Fiji  region, 
including  an  active  monsoonal  trough,  an  enhanced  South 
Pacific  Convergence  Zone  (SPCZ),  two  Tropical  Depressions, 
and Tropical Cyclone (TC) Hettie. 
The hovering of the monsoonal trough and SPCZ over Fiji during 
the early to middle part of January resulted in severe flooding 
that claimed 12 lives and caused major damage in many parts 
of Viti Levu and Vanua Levu. Many roads and bridges including 
the Sigatoka old bridge were destroyed. There was significant 
damage to agricultural crops along the major floodplains. Ba, 
Nadi, and parts of Sigatoka town were flooded. In the case of 
Ba and Nadi, flooding was the worst in over 75 years. School 
facilities  and  homes  in  these  areas  were  without  water  and 
electricity for several days due to broken water pipes. As of  30 
January, the flood related damage cost is F$76.1M.
A  flooded  house  in  Nadi,  Fiji  that  resulted  from  high  rainfall 
during January 2009.
The  January  2009  floods  are  the  worst  natural  disaster 
‘economically’  to  affect  Viti  Levu  since  the  drought  of  1998. 
The title of ‘worst natural disaster’ should probably continue to 
apply to the TC(s) and flooding in late February 1931 when 
The Island
        
Climate Update
A badly damaged bridge in Nadi, Fiji
flooding similar in magnitude to the 2009 event (but including 
the  Rewa  River)  claimed  more  than  200  lives.  There  were 
statements  in  the  media  soon  after  the  recent  flood  that  the 
2009 event was higher than the 1931, 8.37 m above mean sea 
level record at the Rarawai Mill.
Highlights of the month include:
•Seven sites receiving more than 200 mm rainfall in
 
24 hours
•A daily rainfall total of 378 mm on the 13th at
 
Nabouwalu, breaking the record from 1932
•Fourteen stations recording more than 700 mm
 
rainfall
•Seven sites receiving more than 1m of rainfall
•A total monthly rainfall of 1545.1 mm recorded at
 
Monasvu, the highest since records began there in  
 
1980
A complete accounting of the month’s events, climate statistics, 
an  explanation  of  the  cause  of  the  January  flooding,  and 
photographs from across Fiji of the flood damage can be found 
on  the  Fiji  Meteorological  Services  website  (www.met.gov.fj/
index.php).  
Further enquiries about the floods can also be directed to the 
Fiji Meteorological Services by emailing climate@met.gov.fj.