Question: What part of the Grand Cranyon sees rain in the summer?
About the article "Grand Canyon", section "Geography".

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Winter in North Dakota is characterized by cold (below freezing) temperatures and snowfall.
Snow is the main form of winter precipitation, but freezing rain, ice, sleet, and sometimes even rain are all possible during the winter months.
Common storm systems include Alberta clippers or Panhandle hooks, some of which evolve into blizzards.
Annual snowfall averages from 26 inches (66 cm) in the central part of the state to 38 inches (96.5 cm) in the northeast and southwest.
Temperatures as low as −60 °F (−51 °C) have occurred during North Dakota winters.
Spring is a time of major transition in North Dakota.
Early spring commonly sees snowstorms, but by late spring as temperatures begin to moderate the state can experience tornado outbreaks, a risk which diminishes but does not cease through the summer and into the fall as North Dakota lies at the northern edge of Tornado Alley.
Springtime flooding is a relatively common event in the Red River Valley, due to the river flowing north into Canada.
The spring melt and the eventual runoff typically begins earlier in the southern part of the valley than in the northern part.
The most destructive flooding in eastern North Dakota occurred in 1997, which caused extensive damage to Grand Forks.
Summer sees heat and humidity predominate in the east, while hotter and less humid conditions are generally present in the west.
These humid conditions help kick off thunderstorm activity 22–34 days a year.
Summer high temperatures in North Dakota average in the mid 80s (30 °C) in the west to the upper 70s (25 °C) in the east, with temperatures as hot as 121 °F (49 °C) possible.
The growing season in North Dakota usually begins in April, and harvest begins in September and October.
Tornadoes are possible in North Dakota from April through October, but the peak tornado month is July, followed by June and August.
The state averages 13 tornadoes per year.
Depending on location, average annual precipitation ranges from 14 in (35.6 cm) to 22 in (55.9 cm).
Autumn weather in North Dakota is largely the reverse of spring weather.
The jet stream, which tends to weaken in summer, begins to re-strengthen, leading to a quicker changing of weather patterns and an increased variability of temperatures.
By late October and November these storm systems become strong enough to form major winter storms.
Fall and spring are the windiest times of the year in North Dakota. 
The Grand Summer Gala is the railway's largest event.
It features the entire home fleet of locomotives in operation, along with visiting locomotives.
Alongside the standard passenger trains, demonstration freight trains are run, featuring the railway's large fleet of freight and permanent way stock.
The gala also sees the usage of a number of heritage coaches from the Tucktonia railway, albeit not on passenger duties.
All of the locomotives in steam take part and follow each other around the track in a parade lap on the Sunday morning.
Other features of the gala include parades of full-size and miniature steam traction engines, a display of classic cars and a model railway exhibition in our carriage sheds. 
These are the formats and track listings of major single releases of "Summer Rain".
Kent's climate is classified as a humid continental climate in the "Dfa" Köppen climate classification meaning it typically has very warm, humid summers and cold, snowy winters with moderate and variable spring and autumn seasons.
The record high temperature is , set on July 7, 1988, with the record low of recorded January 17, 1982.
During the spring and summer months, thunderstorms are fairly common and the area is susceptible to tornadoes, though the last recorded tornado in Kent occurred in 1973.
Effects from tropical systems can also be felt, usually taking the form of increased humidity, rain, and wind, such as with the remnants of Hurricane Ike in September 2008.
During the winter months, snowfall is common and can occur in large quantities with considerable cloud cover.
Kent is not considered part of the Lake Erie snowbelt, though lake-effect snow does occur at times.
The city is in what is referred to as the "secondary snowbelt", meaning it will receive heavier snowfall totals from lake-effect snow when certain wind directions are more prevalent, but typically sees far less snowfall than areas to the north closer to Lake Erie.
While temperatures below the freezing point are typical in the winter months, thaw periods where temperatures exceed and even are not uncommon in January and February.