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Surface Analysis

SYNOPTIC ANALYSIS • EASTERN NORTH CAROLINA

Surface Analysis

Track fronts, pressure systems and the near-surface weather pattern from Eastern North Carolina to the continental scale.

Official analysis NOAA Weather Prediction Center Fronts • pressure centers • isobars • observations
EASTERN NORTH CAROLINA

Local Surface Overview

Current MRMS radar provides the local Eastern North Carolina view, paired with official WPC surface analyses below.

ENC Radar Overview NOAA/NCEP MRMS composite reflectivity • interactive pan and zoom
Full Radar →
WEATHER PREDICTION CENTER

Current Surface Analyses

Official WPC charts provide the larger-scale context for the fronts and pressure systems affecting the East.

MAP LEGEND

Reading a Surface Chart

Surface analyses identify boundaries between air masses and centers of high and low pressure. The symbols point toward the direction in which a moving front is advancing.

▲ ▲ ▲ Cold Front

Colder air advancing into warmer air. Wind shifts, temperature changes and bands of showers or storms commonly occur near the boundary.

● ● ● Warm Front

Warmer air advancing over cooler air, often accompanied by broader cloud and precipitation areas.

▲ ● ▲ ● Stationary Front

A boundary with little net movement. Persistent weather can develop when moisture repeatedly follows the front.

▲ ● ▲ ● Occluded Front

Forms as a faster cold front overtakes a warm front, typically near a mature low-pressure system.

H High Pressure

Surface pressure maximum; often associated with sinking air, though sensible weather depends on the full pattern.

L Low Pressure

Surface pressure minimum around which fronts and areas of organized precipitation frequently develop.

WPC TOOLS

Explore the Analysis

Use the official WPC tools for interactive viewing, historical charts and short-range surface forecasts.

WHY IT MATTERS

The surface pattern is the starting point

Fronts and pressure systems help explain where air masses are changing and where forcing for clouds, precipitation, wind shifts and temperature changes is concentrated. For Eastern North Carolina, the broader WPC analysis is useful for seeing approaching systems well before they reach the local radar domain.