Climate Climate hazard and extreme events

33 Table 4.1. Income of Phuket Department of Provincial Administration 2004 2005 2006 2007 Agriculture 4,886 4,945 5,529 5,788 Agriculture, Hunting and Forestry 1,642 1,947 2,402 2,537 Fishing 3,244 2,998 3,127 3,251 Non-Agriculture 50,076 45,427 51,599 56,268 Mining and Quarrying 8 Manufacturing 2,037 2,271 2,394 2,556 Electricity, Gas and Water Supply 1,355 1,296 1,460 1,574 Construction 2,457 2,925 2,927 2,999 Wholesale and Retail Trade; Repair of Motor Vehicles, Motorcycles and Personal and Household Goods 4,603 5,089 6,043 6,275 Hotels and Restaurants 25,785 20,766 22,000 23,880 Transport, Storage and Communications 6,614 5,174 7,887 9,173 Financial Intermediation 1,459 1,660 1,924 2,176 Real Estate, Renting and Business Activities 1,424 1,516 1,713 1,923 Public Administration and Defence; Compulsory Social Security 1,155 1,227 1,306 1,432 Education 993 1,172 1,519 1,673 Health and Social Work 821 923 990 1,127 Other Community, Social and Personal Services Activities 1,318 1,359 1,388 1,430 Private Households with Employed Persons 48 49 49 51 Gross Provincial Product GPP 54,962 50,371 57,128 62,055 GPP Per capita Baht 201,339 180,439 200,765 214,621 Population 1,000 persons 273 279 285 289

4.4.3 Climate

Phuket climate is characterized by two seasons. The hot season starts in December and ends in March, with a daily mean temperature average of 28.4 °C and 40mm monthly average of rainfall amount. The rainy season begins in April and lasts until November, with rainfall peaks in May up to 320mm and September up to 400mm. During this season the temperature is comprised between 32 °C for the highest and 23.8°C for the minimum. The daily average temperature during the year is comprised between 23 °C and 34°C. 34 The monthly normal as calculated from the monthly mean of different temperatures during the period from 1980 to 2008 is given in Figure 4.11. Being a coastal station the minimum temperature is slightly higher compared to that of northern stations particularly in winter. Figure 4.11 . Monthly mean normal of temperature; Tmax, Tmin, mean Temperature, Ext. Tmax and Ext. Tmin obtained from the data 1980 to 2008 over Phuket Source: Thailand Meteorological Dept. With respect to monthly normal rainfall it is found that September and October are the peak months followed by August, May, July and June Figure 4.12a. The peak no. of rainy days and the observation of highest rainfall in a day more than 7 cmday is reported mainly during September and October Figure 4.12ac. 35 Figure 4.12. Normal monthly mean rain parameters over Phuket from 1980 to 2008. a total rain b number of rainy days and c maximum rain in 1 day Source: Thailand Meteorological Dept. 36

4.4.4 Climate hazard and extreme events

The coastline of the island is continuously exposed to sea erosion and has to cope with sudden and disastrous events, such as tsunami tidal wave. The 26 December 2004 the earthquake in the Sumatra Island created a massive tsunami tidal wave, which devastated the Andaman Coast. Phuket suffered from disastrous loss of lives, assets and natural resources. 13,065 people died or disappeared during the event; 402 residences were totally destroyed; 550 partially. The utility and facility systems of the island were heavily damaged. In total the overall damages cost more than 13,000.54 million Bahts Strategy for Provincial Development Unit, Phuket Governor’s Office and National Economic and Social Development Board. Strategic plan has been developed to curb the potential impacts of such disasters. Phuket is also very much exposed to irreversible damages on its coral reefs due to high concentration of carbon dioxide emissions in the atmosphere that tends to increase the sea temperature. Reef-building corals are a part of a rich ecosystem that provides resources for the coastal populations. They also serve as buffer against strong waves that erode coastlines during storms. Currently the coral cover is declining at the rate of one to two per cent annually due to destructive fishing, tourism, sedimentation caused by coastal development, eutrophication due to untreated water run-off, dredging and climate change. According to Phuket Marine Biological Centre PMBC, Phuket coastline is seriously endangered by all these interlinked dynamics. According to the Thailand Meteorological Department, the southern part of Thailand is relatively exposed to high risk of tropical storms and typhoon. On top of high-speed winds that can damage the infrastructure, heavy rainfall due to the topography of the area can lead to flooding and contribute to destabilize the slopes. In fact one of the disasters Phuket has to increasingly cope with is landslide occurrence. Uncontrolled human settlements help weaken the slopes and heavy rainfalls help trigger landslides in the zone. The tropical climate participates thereby to the instability of the slopes and as climate change interacts with rainfall events, triggering more intense and more frequent rain amount, landslides are meant to occur and affect more people more frequently. Surrounded by mountains Patong area is especially prone to landslide as about 20 of the area has high to moderate susceptibility to landslide. The area is heavily prone to risk; first the populations living in the toe of the mountain are located within the landslide prone area, while the populations living in the plain area are exposed to flood risk. Adaptation project towards landslide risk mitigation has started to be implemented in the zone.

4.5 Samut Sakhon