Climate - Papua New Guinea

Index

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• Introduction
• Equatorial climate - Madang
• Tropical climate - Port Moresby
• Mountains - Goroka
• Cyclones

Introduction

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Papua New Guinea is an island state, located south of the equator and formed by the eastern part of New Guinea (the western part belonging to Indonesia) plus some smaller islands (including New Britain, New Ireland, Manus and Bougainville).
The climate in Papua New Guinea is hot and humid throughout the year along the coasts and in the plains, while it is progressively cooler, and then colder, as you go up in altitude. In much of the country, covered with dense rainforests, there is no dry season, so we can speak of equatorial climate, while in some inland valleys and along the south coast, there is a relatively dry season from July to September, and therefore the climate is tropical.
The climate is influenced by the monsoon circulation: the northwest monsoon prevails from December to April, and the southeast monsoon from May to October. Usually, each monsoon brings rainfall on the exposed slope, but in many areas, it rains during both the monsoons, so it rains all year round.
Rainfall typically ranges from 2,000 to 4,000 millimeters (80 to 160 inches) per year, with some higher peaks on the most exposed slopes, where it reaches as high as 7/8 meters (23/26 feet) per year, while it drops to 1,000/1,500 mm (40/60 in) on the southern coast, overlooking the Gulf of Papua and the Coral Sea.
On the coasts, the temperatures are high and stable throughout the year in the north, around 30/32 °C (86/90 °F) during the day, while in the south, located farther from the Equator, they decrease a bit (around 2 degrees Celsius) in the southern hemisphere winter, from June to September.

Equatorial climate

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Madang

As mentioned, temperatures along the coasts are high throughout the year, and in particular, they are very stable in the areas with an equatorial climate. Here are the average temperatures of Madang, located at 5 degrees south latitude, on the north-eastern coast of New Guinea.

In Madang, 3,500 mm (138 in) of rain fall per year, with a maximum of 430 mm (17 in) in April and a minimum of 120 mm (4.7 in) in August, in fact, as mentioned, we are in the area that has an equatorial climate. Here is the average precipitation.

The amount of sunshine in Madang is generally decent, but not exceptional; however, it is a little higher in the least rainy period, from June to October. Here are the sunshine hours.

The sea is always warm enough for swimming throughout the country, and in the north, near the equator, the sea temperature is more stable, as we can see in the following table.

To the east of the eastern part of New Guinea, which constitutes the largest portion of the country, the islands (including New Ireland, New Britain and Bougainville) are very rainy throughout the year as well. In general, the rains are most abundant from December to April, but not everywhere: in Lae, facing south-east in the Huon Gulf, the rains are most abundant in July and August, when more than 500 mm (20 in) fall per month.

Tropical climate

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Port Moresby

As mentioned, in the south the temperature decreases more evidently from June to September. The capital, Port Moresby, is located at 9 degrees south latitude, on the coast.
At night it never gets cold, however, the temperature can sometimes drop to 19/20 °C (66/68 °F) from June to September.
At the end of the dry season, in October and November, there can be very hot periods, but some very hot days can also occur in the rainy season, from December to March. As a result, on the hottest days, the temperature can reach 35/36 °C (95/97 °F) from October to March.
Here are the average temperatures.

Port Moresby is located in the southern area, which, as mentioned, is less rainy and more sheltered, so much so that it receives only 1,000 mm (40 in) of rain per year, with a relatively dry period from May to November, when rainfall drops below 70 mm (2.8 in) per month; in particular, the rains are scarce from June to October. Here is the average precipitation.

Being that the rains are less frequent, the amount of sunshine in Port Moresby is higher than in other areas of the country.

In the southernmost part, where the capital is located, the sea becomes a bit less warm from July to October, as we can see in the following table.

Mountains

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The interior of the mainland (eastern New Guinea) is crossed by mountains: in the north, we find the Victor Emanuel Range and the Bismarck Mountains, the latter culminating in Mount Wilhelm, 4,509 meters (14,793 feet) high, while in the south, we find the Owen Stanley Mountains, whose highest peak is Mount Victoria, 4,038 meters (13,248 feet) high.
At 1,500 meters (5,000 feet) of altitude, the temperature is pleasant: cool at night and warm during the day.

Goroka

Here are the average temperatures of Goroka, located at 1,600 meters (5,2520 feet) above sea level, in the Eastern Highlands province.

In Goroka, 1,700 mm (68 in) of rain fall per year; there is a relatively dry season from June to August, when, however, some showers can still occur.

The sun in the mountainous areas shines less often than on the coasts, and the sky is often cloudy.

Above 3,500 meters (11,500 ft), the forest is replaced by a sparse mountain vegetation: here, the cold is constant and sometimes it can even snow.
From the mountains, numerous rivers flow, such as the Sepik and the Fly, which in lowland areas, often at great distance from the mouth, give rise to marshes and swamps, where mangroves and gallery forests grow.

Tropical cyclones

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Papua New Guinea can be affected by tropical cyclones of the South Pacific. Typically, cyclones are formed from November to mid-May, although they are more likely from late November to mid-April. The part of the country that is directly affected is the center-south. The map below is an indication of the areas that have been affected in the past. The northern areas, however, may be partly affected, with an increase in wind, clouds, and waves.



The climate of Papua New Guinea is also influenced by the so-called ENSO cycle. In El Niño years, the rainy season is warmer and drier than normal, and the monsoon arrives often late, while the dry season is cooler than normal in the south. On the other hand, in La Niña years, the rainy season from December to April is more intense than normal and can lead to flooding, while the dry season is warmer than normal in the south. During neutral phases (neither El Niño nor La Niña), however, it's more likely for cyclones to form.



When to go and what to pack in Papua New Guinea