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The climate of Alaska is determined by average temperatures and precipitation received statewide over many years. The extratropical storm track runs along the Aleutian Island chain, across the Alaska Peninsula , and along the coastal area of the Gulf of Alaska which exposes these parts of the state to a large majority of the storms crossing the ...
Anchorage has a frost-free growing season that averages slightly over one hundred days. Average January low and high temperatures at Ted Stevens Anchorage International Airport (PANC) are 11 / 23 °F (−11.7 / −5.0 °C) with an average winter snowfall of 75.59 inches, or 1.92 meters. Farther afield at the Campbell Airstrip is another weather ...
Climate charts provide an overview of the climate in a particular place. The letters in the top row stand for months: January, February, etc. The bars and numbers convey the following information: The blue bars represent the average amount of precipitation (rain, snow etc.) that falls in each month. The blue numbers are the amount of ...
The blue numbers are the amount of precipitation in either millimeters (liters per square meter) or inches. The red numbers are the average daily high and low temperatures for each month, and the red bars represent the average daily temperature span for each month. The thin gray line is 0 °C or 32 °F, the point of freezing, for orientation.
A climograph is a graphical representation of a location's basic climate. Climographs display data for two variables: monthly average temperature; monthly average precipitation. [1] These are useful tools to quickly describe a location's climate.
Sea ice melted, kids swam in unusually warm water and Anchorage hit 90°F for the first time as Alaska becomes America's starkest example of climate change. Alaska records its warmest month ever ...
Freezing temperatures and snowfall can occur during any month of the year. [33] As of 2023, Utqiagvik falls within USDA Hardiness Zone 2B. [35] Regarding precipitation, Utqiagvik has a desert climate and averages less than 6 in (150 mm) "rainfall equivalent" per year. One inch of rain has an estimated water content equal to 12 in (30 cm) of snow.
Also, precipitation measurements are difficult, especially for snow, as the gauge must empty itself between observations. For present weather, all phenomena that do not touch the sensor, such as fog patches, remain unobserved. [1] The change from manual observations to automatic weather stations is a major non-climatic change in the climate ...