Maple Ridge Climate & Monthly Temperature Overview – Canada

Climate Overview

Maple Ridge, British Columbia, experiences a temperate climate influenced by its proximity to the Pacific Ocean. The region is characterized by mild, wet winters and warm, dry summers. Temperatures typically range from an average low of 0°C (32°F) in January to an average high of 25°C (77°F) in August. Precipitation is abundant throughout the year, with the wettest months being November and December, when rainfall can exceed 200 mm (8 in). Snowfall is common during the winter months, but accumulations are generally light and temporary.

Seasonal Weather

Winter: Winters in Maple Ridge are generally mild, with temperatures rarely falling below freezing. However, periods of cold and snowy weather can occur, especially in January and February. Snowfall is infrequent but can accumulate during heavy snowfall events.

Spring: Spring arrives in Maple Ridge around March, bringing with it increasing temperatures and longer daylight hours. April and May see an increase in precipitation, with occasional showers and thunderstorms. The vegetation begins to emerge, and wildflowers come into bloom during this time.

Summer: Summers in Maple Ridge are warm and mostly dry, with little humidity. Temperatures reach their peak in July and August, when daily highs average around 25°C (77°F). The region enjoys plenty of sunshine, with clear skies prevailing for most of the season.

Fall: Autumn sets in during September, bringing cooler temperatures and increased precipitation. The leaves on deciduous trees begin to turn brilliant shades of red, orange, and yellow. October and November are generally wet and windy, with occasional cold snaps.

Average Temperature in Maple Ridge, Canada

Maple Ridge, a city in British Columbia, Canada, experiences a temperate climate with distinct seasonal variations. The average annual temperature in Maple Ridge is approximately 10.5 degrees Celsius (50.9 degrees Fahrenheit). Summers in Maple Ridge are generally warm and dry, with average temperatures ranging from 15.6 to 22.8 degrees Celsius (59.9 to 73.1 degrees Fahrenheit) in July and August. Winters, on the other hand, are mild and humid, with average temperatures hovering around 0 to 5.8 degrees Celsius (32 to 42.4 degrees Fahrenheit) from December to February.

The average monthly temperature in Maple Ridge varies considerably throughout the year. January, the coldest month, has an average temperature of 2.4 degrees Celsius (36.3 degrees Fahrenheit). In contrast, July, the warmest month, boasts an average temperature of 18.7 degrees Celsius (65.7 degrees Fahrenheit). The city experiences significant precipitation throughout the year, with an average annual rainfall of 1,537 millimeters (60.5 inches). Rainfall is particularly heavy during the winter and early spring months, while summers tend to be drier.

Cloud Types

Maple Ridge is located in the Pacific Northwest, which experiences a variety of cloud types throughout the year. Common cloud types include cirrus, cumulus, stratus, and nimbus. Cirrus clouds are thin, wispy clouds that appear high in the sky. Cumulus clouds are puffy clouds with flat bases that often indicate fair weather. Stratus clouds are uniform, gray clouds that cover the entire sky and can produce drizzle or light rain. Nimbus clouds are dark, rain-producing clouds that often bring showers or thunderstorms.

Cloud Cover

Cloud cover in Maple Ridge varies depending on the time of year. During the winter months, the area experiences more cloud cover due to frequent storms and precipitation. The average cloud cover during this time is around 80%. In the summer months, cloud cover decreases to around 50% as the weather becomes drier and sunnier. However, even during the summer, clouds can still appear and bring rain or thunderstorms. The presence of clouds affects the temperature and humidity in Maple Ridge. On cloudy days, temperatures tend to be cooler and the humidity is higher. On clear days, temperatures can reach higher levels, and the humidity is lower.

Annual Precipitation

Maple Ridge’s annual precipitation averages approximately 1,600 millimeters (63 inches), making it one of the wetter regions in British Columbia. The precipitation is relatively evenly distributed throughout the year, with slightly higher amounts during fall and winter. The wettest month is typically November, with an average of 225 millimeters (8.9 inches) of rainfall. July and August are the driest months, with an average of 50 millimeters (2.0 inches) of rainfall.

Seasonal Precipitation

In winter, precipitation often occurs as snowfall, especially in higher elevations. The average annual snowfall in Maple Ridge is 50 centimeters (20 inches). However, the amount of snowfall varies significantly from year to year, with some winters experiencing much heavier snowfall than others. Spring and fall typically bring a mix of rain and snow, with temperatures fluctuating around the freezing mark. Summer is generally the driest season, with warm and sunny weather. The warm temperatures and infrequent precipitation during summer create ideal conditions for outdoor activities such as hiking, biking, and swimming.

Rainfall Patterns in Maple Ridge, Canada

Maple Ridge, a city located in the Lower Mainland region of British Columbia, Canada, experiences a temperate oceanic climate with significant rainfall throughout the year. The city’s proximity to the Pacific Ocean and the Coast Mountains play a crucial role in shaping its precipitation patterns. During the winter months (October to March), the region is frequently impacted by Pacific storms that bring heavy rainfall and occasional snowfall. The wettest period typically occurs in November and December, with an average rainfall of over 200 mm each month.

Seasonality and Variability of Rainfall

Rainfall in Maple Ridge exhibits a distinct seasonality, with a marked contrast between the wet and dry seasons. The summer months (June to September) are generally drier, with average rainfall ranging from 50 to 100 mm per month. During this period, the influence of the Pacific storms diminishes, and precipitation is primarily associated with convective thunderstorms or occasional frontal systems. However, variations in rainfall patterns can occur from year to year due to factors such as El Niño-Southern Oscillation (ENSO) or changes in atmospheric circulation patterns. During strong El Niño years, for instance, Maple Ridge may experience reduced rainfall during the winter months. Conversely, during La Niña years, heavier rainfall is more likely.

Historical Snowfall Records and Trends

Maple Ridge, located in British Columbia, Canada, has experienced significant snowfall throughout its history. The average annual snowfall in the city is 14.5 centimeters, with the highest recorded snowfall occurring in the winter of 2008-2009, when 179 centimeters fell. However, snowfall patterns have fluctuated over the years, influenced by factors such as La Niña and El Niño weather events. In recent years, Maple Ridge has witnessed a gradual increase in snowfall, attributed to a rise in average winter temperatures causing more precipitation to fall as snow instead of rain.

Snowfall Impacts and Management

Snowfall in Maple Ridge has both positive and negative impacts. On the positive side, snow provides snowpack for skiing, snowshoeing, and other winter recreational activities. It also helps water reservoirs by gradually releasing snowmelt during warmer months. On the negative side, snowfall can lead to road closures, power outages, and transportation delays. To mitigate these impacts, Maple Ridge has developed a comprehensive snow removal plan. This plan involves snow plowing, salting, and sanding operations to ensure safe and accessible roadways. Additionally, the city provides snow removal services to residents who are unable to clear snow themselves, ensuring the safety and well-being of its citizens during winter weather events.

Sunrise and Sunset Times

The timing of sunrise and sunset in Maple Ridge, Canada varies significantly throughout the year, influenced by the Earth’s orbit and tilt. During summer months, typically from May to July, days are longer, with sunrise occurring earlier and sunset later. On the summer solstice, around June 21, Maple Ridge experiences its longest day of the year, with sunrise around 5:30 AM and sunset around 9:30 PM. In contrast, winter days are shorter, with sunrise occurring later and sunset earlier. On the winter solstice, around December 21, Maple Ridge has its shortest day of the year, with sunrise around 8:00 AM and sunset around 4:30 PM.

Seasonal Variations

The amount of sunlight Maple Ridge receives also varies seasonally. In the spring and summer, the sun is higher in the sky, resulting in more direct sunlight and longer periods of daylight. This increased sunlight contributes to warmer temperatures and longer days, making it an ideal time for outdoor activities and enjoying the outdoors. However, during the fall and winter, the sun is lower in the sky, leading to less direct sunlight and shorter days. As a result, temperatures drop, and nights become longer, encouraging hibernation and cozy indoor activities.

Sunset Moon

The captivating beauty of the sunset moon in Maple Ridge, Canada is a mesmerizing sight. As the sky transforms from radiant hues of pink and orange to a deep indigo, the moon gracefully emerges, casting an ethereal glow over the landscape. The gentle beams dance upon the sparkling surface of the Fraser River, creating a shimmering tapestry of light. The silhouette of towering trees, reaching towards the heavens, serves as a magnificent backdrop for this celestial spectacle, casting long shadows that dance with the wind.

Moonlight Landscapes

Beneath the moon’s silvery glow, Maple Ridge transforms into a mystical wonderland. The towering mountains become silent guardians, their snow-capped peaks illuminated by the moonlight. The dense forests whisper secrets, their branches adorned with shimmering dew drops. The city lights, twinkling in the distance, create a surreal panorama that blends the natural and urban worlds. The crisp air carries the scent of blooming wildflowers and the gentle chorus of crickets, creating a symphony that soothes the soul.

Seasonal Variations in Humidity

In Maple Ridge, Canada, humidity levels exhibit a distinct seasonal pattern. During the winter months (December to February), the average relative humidity hovers around 80-90%. The cold temperatures and lack of precipitation contribute to this high humidity, which can often lead to fog and drizzle.

In the spring (March to May), humidity levels begin to decline slightly as temperatures rise and precipitation increases. The average relative humidity during this period typically ranges from 70-80%. This moderate humidity provides comfortable conditions for outdoor activities.

Summer and Fall Humidity

Summer in Maple Ridge (June to August) brings warm and humid weather. The average relative humidity during this time is around 70-80%, with occasional dips into the 60s. While the heat can be uncomfortable for some, the humidity helps to moderate the temperatures and prevent extreme heat.

In the fall (September to November), humidity levels gradually decrease as temperatures cool. The average relative humidity during this period ranges from 60-70%. The lower humidity combined with the crisp autumn air creates ideal conditions for outdoor pursuits, such as hiking and biking.

Wind Patterns in Maple Ridge, Canada

Maple Ridge, British Columbia, Canada, is situated on the Fraser River, surrounded by mountains and the Salish Sea. The city’s topography significantly influences its wind patterns. The prevailing wind direction in Maple Ridge is from the southwest, bringing moist Pacific air into the area. This wind typically occurs during the summer months when the low-pressure systems over the Gulf of Alaska pull air northward.

Seasonal Wind Variations

During the winter months, the prevailing wind direction shifts to the northeast as high-pressure systems over the Arctic bring cold, dry air southward. These winds can be particularly strong, especially during the early morning hours. Additionally, local mountain ranges can channel winds, creating microclimates within the city. For example, the Golden Ears mountains to the northeast of Maple Ridge often deflect winds, resulting in calmer conditions in the city center.

Spring (April-May)

Springtime in Maple Ridge offers a vibrant display of colors as flowers bloom in abundance. Temperatures rise to the mid-teens, making it an ideal time for outdoor activities. The city’s many parks and trails come alive with hikers, bikers, and picnickers. The popular Golden Ears Lookout Trail provides stunning views of the snow-capped Golden Ears Mountains. Additionally, the Kanaka Creek Regional Park offers canoeing and kayaking opportunities in its pristine waterways.

Summer (June-August)

Summer in Maple Ridge is characterized by warm, sunny days and balmy nights. Temperatures typically reach the low twenties, making it a perfect time for swimming, fishing, and water sports. The city’s outdoor pools and spray parks provide a refreshing escape from the heat. The Maple Ridge Farmers’ Market, held every Saturday from June to October, showcases local produce, crafts, and music. For a unique cultural experience, visit the Haney House Museum, which preserves the heritage of the region’s early settlers.

Potential for Solar Energy in Maple Ridge

Maple Ridge, situated in southwestern British Columbia, possesses promising prospects for solar energy utilization. The region experiences abundant sunshine, averaging 2,200 annual sunshine hours. This favorable solar resource, coupled with the city’s commitment to sustainability, makes Maple Ridge an ideal location for embracing solar energy.

Residential and Commercial Applications

Solar photovoltaic (PV) systems are gaining popularity among homeowners and businesses in Maple Ridge. Residential rooftop systems allow homeowners to reduce their electricity bills and enhance their energy independence. Businesses can also benefit from solar PV by lowering operating costs and showcasing their environmental consciousness. Additionally, the local government offers financial incentives, such as rebates and property tax exemptions, to encourage the adoption of solar energy in the community.

Topography of Maple Ridge, Canada

The topography of Maple Ridge, Canada, is characterized by rolling hills, river valleys, and forested mountains. The city is situated at the confluence of the Fraser and Pitt Rivers, which have carved deep valleys into the surrounding landscape. The valleys are flanked by steep hillsides and mountains, including the Golden Ears Mountains to the north and the Coast Mountains to the west. The highest point in Maple Ridge is Mount Robie Reid, with an elevation of 1,250 meters (4,100 feet).

The topography of Maple Ridge has a significant impact on the city’s climate, hydrology, and ecology. The steep slopes and mountains create a rain shadow effect, which results in lower precipitation levels in Maple Ridge than in other parts of the Lower Mainland. The Fraser and Pitt Rivers provide a vital source of water for the city and its surrounding communities, and they also support a diverse ecosystem of fish and wildlife. The forested mountains are home to a variety of plant and animal species, and they provide recreational opportunities for residents and visitors alike.

Abbotsford International Airport (YXX)

Located approximately 25 kilometers (15 miles) southeast of Maple Ridge, Abbotsford International Airport (YXX) is the nearest major airport. It offers a wide range of domestic and international flights, with direct connections to major cities across Canada and the United States. The airport is well-connected to Maple Ridge by public transportation, including buses and taxis. The journey by car takes approximately 30 minutes, depending on traffic conditions.

Vancouver International Airport (YVR)

While Abbotsford International Airport is the closest airport, Vancouver International Airport (YVR) is also a convenient option for travelers. Located approximately 45 kilometers (28 miles) southwest of Maple Ridge, YVR is Canada’s second-busiest airport. It offers a more extensive selection of flights, including international destinations in Europe, Asia, and South America. Although the journey from YVR to Maple Ridge is slightly longer (approximately 45 minutes by car), the airport offers a wider range of amenities and transportation options, including the Canada Line rapid transit system.

History of Maple Ridge

Maple Ridge is a city located in British Columbia, Canada, about 40 kilometers northeast of Vancouver. The area has a rich history dating back to the pre-colonial era, when it was inhabited by the Katzie First Nation. European settlers began arriving in the mid-1800s, and the city was officially incorporated in 1912.

During the early 1900s, Maple Ridge was a thriving agricultural community, known for its dairy and poultry farms. The construction of the Haney Bridge in 1929 connected the city to Coquitlam and New Westminster, leading to increased development and population growth.

Geography and Climate

Maple Ridge is situated in a scenic valley at the confluence of the Fraser and Alouette rivers. The city is surrounded by mountains and forests, offering a beautiful natural backdrop. The climate is temperate, with warm summers and mild winters. The average temperature in July is 21 degrees Celsius, while the average temperature in January is 2 degrees Celsius.

Maple Ridge is a diverse community with a population of over 80,000 people. The city is home to a wide range of amenities, including schools, parks, recreation facilities, and shopping centers. Maple Ridge is a great place to live, work, and raise a family.