March 2018 Nor’easter
March 2018 Nor'easter
Overview
In March 2018, a powerful late-season nor'easter brought heavy snow to the High Country, demonstrating that significant winter weather can occur well into spring in the mountains. The storm dropped over 20 inches of snow at higher elevations, with heavy, wet snow causing widespread tree damage and power outages across the region.
The March timing made this storm particularly impactful. Trees that had begun leafing out were vulnerable to the weight of wet snow. Power lines, already under stress from spring conditions, failed under the snow load. The storm served as a reminder that winter in the High Country doesn't follow the calendar and that March can bring significant snow events.
Key Statistics
Impact and Damage
Heavy, Wet Snow
The March timing and storm characteristics created particularly damaging snow:
- High Water Content: Warmer temperatures meant snow had high moisture content
- Heavy Weight: Each inch of this snow weighed much more than typical winter snow
- Tree Stress: Weight of snow combined with spring conditions caused extensive tree damage
- Accumulation on Everything: Wet snow stuck to and accumulated on all surfaces
Tree Damage and Power Outages
- Extensive tree damage across the region from heavy snow weight
- Trees with early leaf buds particularly vulnerable to damage
- Thousands lost power as trees fell on power lines
- Power restoration took several days for many areas
- Damage to tree canopy visible for months afterward
Travel Disruption
- Roads quickly became snow-covered and hazardous
- Many residents caught off-guard by late-season snow
- School closures throughout the region
- Business closures as conditions deteriorated
- Spring break travel plans disrupted for many
Higher Elevations Hit Hardest
- Areas above 3,500 feet received heaviest snowfall
- Beech Mountain, Blowing Rock, Banner Elk areas: 20+ inches
- Boone area: 15-20 inches
- Lower elevations saw less snow or rain/snow mix
Meteorological Context
Nor'easter Development
The storm was a classic nor'easter that tracked up the coast:
- Low pressure system developed off the Carolina coast
- System tracked northward along the coastline
- Drew Atlantic moisture inland
- Cold air in place over mountains allowed for heavy snow
- Northeasterly winds gave the storm its name
March Snow Characteristics
Why March snow is different from January snow:
- Higher Sun Angle: More solar radiation during day
- Warmer Temperatures: Temperatures near or just below freezing
- High Moisture Content: Air holds more moisture in March
- Wet Snow: Results in heavy, sticky accumulation
- Rapid Melting: March snow often melts quickly once storm passes
Spring Storm Pattern
The 2018 storm fit a pattern of significant late-season events:
- Mountains often see significant snow into March and even April
- Late-season coastal lows can produce major snowfalls
- “Spring” winter storms can rival mid-winter events for snow amount
- Timing catches people off-guard who have moved on mentally to spring
Why March Snow Matters
Ecological Impact
- Early Bloomers: Plants that had begun blooming suffered damage
- Wildlife: Birds and animals already in spring patterns faced challenges
- Tree Damage: Damaged trees more vulnerable to disease and insects
- Spring Activities Delayed: Maple syrup season, early crops affected
Human Impact
- Many had already switched to spring tires, summer wardrobes
- Snow removal equipment sometimes already put away
- Mental adjustment from spring back to winter conditions
- Tourism impacts as spring break visitors encountered winter
- Reminder that winter gear should remain accessible through March
Infrastructure Stress
- Power grid stressed by combination of wet snow and early spring conditions
- Road crews had to re-mobilize winter equipment
- Salt and sand supplies often running low by March
- Budget impacts as winter weather extended into fiscal year end
Historical Context
High Country's March Snow History
Significant March snowstorms are part of High Country history:
- March 1993: The legendary “Storm of the Century” struck in mid-March
- March 2018: This nor'easter brought 20+ inches
- March snow events occur every few years
- April snow is not unheard of at higher elevations
- Last freeze typically doesn't occur until late April or early May
Climate and Seasonal Transitions
Understanding spring snow in context:
- High Country's elevation means extended winter season
- Transition from winter to spring often has back-and-forth pattern
- Warm spells followed by winter returns are normal
- Old timers' saying: “Don't put winter clothes away until Mother's Day”
2018 in Context: A Wet Year
The March 2018 nor'easter was just one event in an exceptionally wet year:
- 2018 became the wettest year on record for the High Country
- Approximately 93 inches of precipitation vs. 59-inch average
- Seven major precipitation events during the year
- March snow contributed to annual total
- Hurricane Florence remnants later in September added more
- Pattern of intense precipitation events separated by dry periods
Lessons and Preparedness
Never Too Early to Put Winter Away
The 2018 storm reinforced important lessons:
- Keep winter clothing accessible through April in High Country
- Don't switch to summer tires too early
- Maintain emergency supplies into spring
- Be prepared for power outages from spring snow
- Have backup heat sources available
Tree and Property Protection
- Trim trees near power lines year-round
- Remove dead or damaged branches before they fail
- Consider tree species that handle wet snow better
- Have tree service contacts ready for emergencies
Article researched and compiled by Kenneth Reece, WataugaOnline.com
Data sources: National Weather Service, North Carolina State Climate Office, and local reports.
Last updated: November 2025





