Learn The Layers
Explore explainers on smog, wildfire weather, flooding, coastal hazards, and the terrain that shapes Southern California forecasts.
Category
Foundational explainers for how Los Angeles and Southern California weather actually works, from mountains and microclimates to weather versus climate.
On a typical July afternoon Woodland Hills runs about 21 degrees hotter than Santa Monica. This guide compares the beach, Westside, Downtown, the Valley and Pasadena, with the numbers behind each.
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Los Angeles sits below an unusual east-west mountain system that lifts ocean air into rain and snow on one side and leaves a dry rain shadow on the other, which is why the coast, basin, foothills, and desert can feel like different climates on the same afternoon.
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Weather is the atmosphere right now, and climate is the statistical pattern behind decades of days like it. Southern California is one of the clearest places in the country to see both operating side by side.
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A watch means conditions are favorable for a hazard and it is time to prepare; a warning means the hazard is occurring or imminent and it is time to act. Here is how that plays out across LA fire, flood, surf, wind, and heat alerts.
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Relative humidity is a percentage that shifts with the thermometer, while dew point is a steadier read on actual moisture, which is why an 85% humidity morning in Santa Monica can feel nothing like a sticky monsoon afternoon inland.
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Los Angeles has so many microclimates because ocean distance, elevation, mountain terrain, urban surfaces, and wind exposure all change sharply and independently within a single county.
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Los Angeles gets almost all its rain between November and March because a single Pacific high pressure system shifts north in summer and south in winter. The same mechanism explains four other Mediterranean-climate coastlines worldwide.
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The San Gabriel, San Bernardino, and San Jacinto Mountains wring the rain out of Pacific storms before that air ever reaches the Antelope Valley, Mojave Desert, or Coachella Valley, leaving those deserts in a persistent rain shadow.
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The Los Angeles sea breeze is a daily, sun-driven wind that turns onshore each afternoon because inland land heats much faster than the Pacific Ocean.
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A falling barometer means rising air and an approaching low pressure system, one of the most reliable storm signals there is. In Los Angeles it still needs a map, a forecast, and a time window to mean anything specific.
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The jet stream is the upper-level wind current that decides whether Pacific storms track into California or get deflected away. Its ridges and troughs, not the calendar, set the region's wet and dry stretches.
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Seismologists have found no reliable weather pattern that predicts an earthquake. The Southern California myth persists mainly because a hot, still day is easy to remember after a notable quake.
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Why the coast wakes up gray, the difference between fog, mist, and haze, and the seasonal marine layer patterns behind May Gray and June Gloom.
May Gray and June Gloom are the seasonal peak of LA's marine layer, driven by cold coastal water and weak inland heating. Here's why the coast stays gray while inland valleys warm up, and when the pattern typically breaks.
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Fog and mist are both suspended water droplets, distinguished mainly by how far you can see through them, while LA haze is dry particulate from smog, smoke, or dust that forms independent of humidity.
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The Los Angeles marine layer is cool, moist ocean air trapped beneath a warm inversion cap, and it explains why the coast can be gray at 8 a.m. while inland neighborhoods are already sunny.
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The Catalina Eddy is a shallow counterclockwise circulation in the Southern California Bight that can deepen and spread LA's marine layer well beyond its usual reach, producing grayer, cooler mornings than the everyday cycle.
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Southern California can hit 90°F on land while the ocean sits near 58°F just offshore. Coastal upwelling, driven by wind and the Coriolis effect, explains the gap and why it peaks in late spring and early summer.
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How photochemical smog forms, why temperature inversions trap it in the basin, and how ground-level ozone builds through the day.
Los Angeles smog is photochemical: sunlight converts nitrogen oxides and VOCs from vehicles and industry into ground-level ozone over several hours, which is why it often peaks inland in the afternoon.
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A temperature inversion places warmer air above cooler surface air, shutting off the vertical mixing that would otherwise let Los Angeles smog, smoke, and haze disperse.
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Ground-level ozone is an invisible gas that forms when sunlight reacts with vehicle and industrial emissions over several hours, which is why it usually peaks inland and in the afternoon rather than at the coast in the morning.
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A No-Burn Day restricts residential wood burning when calm winter weather is expected to trap fine particle pollution across the South Coast Air Basin.
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Los Angeles became the smog capital of America through a specific stack of factors: a mountain-ringed basin, the country's earliest mass car dependence, and near-daily inversions. Here is how that combination was discovered and what has changed since.
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The Air Quality Index looks like one number, but it is actually five separate pollutant scores with only the worst one reported. Understanding that rule explains almost every confusing AQI reading in Southern California.
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PM2.5 is a size category of airborne particles small enough to reach deep into the lungs, and it is usually the pollutant driving Los Angeles's AQI number during wildfire smoke.
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Smog, wildfire smoke, and fog can look nearly identical over Los Angeles, but they differ in smell, timing, and season, and a 30-second AQI check settles what a photo cannot.
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Wildfire smoke filters out shorter blue wavelengths and lets longer red and orange light through, the same physics behind a vivid sunset. But an orange sky says nothing about the PM2.5 level you're actually breathing.
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The Santa Ana wind mechanism, red flag warnings, and the debris flows and mudslides that follow a Southern California wildfire.
Santa Ana winds are dry offshore winds that descend from the Great Basin through Southern California mountain passes, warming and drying as they go and turning any spark into a fast-moving wildfire risk.
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A Fire Weather Watch flags critical fire conditions that could develop soon, while a Red Flag Warning means those conditions are already underway or imminent. Here is how NWS Los Angeles/Oxnard and San Diego use each product.
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A burned Southern California hillside can lose its ability to absorb water in minutes of intense rain, sending a fast, boulder-carrying slurry down canyons toward homes below. Here is how the hazard forms and what actually keeps people safe.
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Los Angeles hillsides can fail after rain when water raises pore-water pressure and weakens steep soil, with risk amplified by fire damage, geology, and past saturation.
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A Wind Advisory means gusts of 45 to 57 mph; a High Wind Warning starts at 58. Here is how to read LA's wind alerts, and why a canyon or pass can be far windier than the forecast headline suggests.
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Intense SoCal wildfire heat can lift a smoke plume high enough to form a true water cloud on top of it. When that cloud glaciates and starts producing lightning, fire crews call it a pyrocumulonimbus, and it is a sign of dangerous, erratic fire behavior.
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Most fire whirls on a Southern California wildfire are small, brief spinning columns of flame and ash. A rare few, given the right terrain, wind, and fuel, grow into far more dangerous fire tornadoes.
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Atmospheric rivers, El Niño versus La Niña, and why flash flooding hits Los Angeles, Long Beach, Orange County, and Palm Springs so fast.
Most LA addresses show FEMA Zone X, yet a UC Irvine study puts up to 874,000 people in a foot of water in a 100-year flood. This guide shows how to check your address on three maps and what each one misses.
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San Diego averages 9.79 inches of rain a year, Downtown LA 14.25 and Pasadena 20.08. This guide lists normals and 2025-26 totals for 20-plus cities and explains why one storm can drop 2 inches in one place and 12 in another.
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Downtown Los Angeles averages 14.25 inches of rain a year, but the typical year falls short and a few huge winters make up the difference. The 2025-26 season finished near 138% of normal.
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Atmospheric rivers carry the moisture behind most of Southern California's biggest rain and mountain snow events. Duration, orientation, and terrain, not the label alone, decide whether one soaks the region gently or floods it.
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El Niño and La Niña are opposite phases of the same tropical Pacific pattern that shift the odds of a wet or dry Southern California winter, but neither one locks in the outcome.
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Los Angeles can go from dry pavement to a dangerous flash flood in well under an hour. Steep watersheds, paved neighborhoods, and burn scars are why the basin reacts so much faster than the storm outside your window suggests.
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Long Beach has almost no natural slope to move floodwater, so heavy rain relies entirely on storm drains that a high tide can slow down. Here is what makes this stretch of coast flood differently than the rest of LA County.
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Orange County does not have one flash-flood story. Foothill canyons, flat suburban grids, and low coastal streets each flood for a different reason, and the alert you need depends on which one you are standing in.
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Palm Springs looks bone dry most of the year, but steep canyons draining the San Jacinto and San Bernardino Mountains can turn a normally empty wash into a fast, muddy torrent within minutes of a monsoon cell or winter storm.
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Lightning threatens Southern California beaches, mountains, and deserts even outside the heaviest rain, so the safest response is to shelter the moment thunder is heard.
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Collecting rainwater from your own roof is legal in California, though larger systems, potable-use plans, and local building codes can still bring in permit requirements.
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A wet Los Angeles winter is not weeks of drizzle. It is a handful of Pacific storms, often just five to eight multi-day systems, that deliver most of the season's total rainfall in bursts.
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A Pineapple Express is the Hawaii-sourced version of an atmospheric river, warmer and wetter than a typical Pacific storm, with a snow level too high to favor mountain snow.
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A bomb cyclone describes how fast a storm intensified offshore, a pressure drop of at least 24 millibars in a day, not how much damage it will do once it reaches Southern California.
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Flood and flash flood alerts sound similar but describe very different timelines. Here is how LA's five NWS flood products differ, and which one demands you move immediately.
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Pasadena floods differently than the rest of Los Angeles because it sits right where the steep San Gabriel Mountains meet the city grid. Here is how mountain-front watersheds, the Arroyo Seco, Eaton Canyon, and burn scars combine to create a fast-moving, sometimes debris-laden hazard.
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Santa Monica does not have steep canyons or a slow-draining flat basin. It has a dense, paved city grid that drains straight toward the ocean, plus canyon runoff from above and a tide that can slow the exit below. Here is how those pieces combine into fast, local flooding.
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Ventura floods where two rivers, a large agricultural watershed, and the open coast all meet at once. Here is how mountain runoff, burn-scar debris, and high tide or surf at the river mouths combine into a fast-developing local hazard.
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A thunderstorm over a ridge you cannot see can fill a Joshua Tree wash below your boots in minutes. Hardpan soil, bare rock, and remote canyons with no cell signal make this a different flash flood risk than any paved desert town nearby.
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The North American monsoon pulls Gulf of California moisture into the Southwest each summer, occasionally triggering desert thunderstorms near Palm Springs and Joshua Tree while coastal Los Angeles stays largely untouched.
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On the September 24, 2026 U.S. Drought Monitor map, about 23% of California was in Moderate Drought and Los Angeles County was drought-free. This guide explains what the map measures, why Southern California can differ and where to check the current status.
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Southern California gets barely more rain in an average year than parts of the Mojave, and it imports most of its water from hundreds of miles away. That combination, not any single dry winter, is why the region is structurally built for drought.
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How thunderstorms, lightning and hail form, why Los Angeles sees so few of them, and how to read cumulus, lenticular and other clouds over Southern California.
Cool Pacific air keeps the Los Angeles coast and basin thunderstorm-free most of the year, but winter storms, summer monsoon surges, and rare tropical remnants still bring real lightning risk, especially over the mountains.
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Every thunderstorm needs moisture, instability, and lift stacked in the same place at once. Coastal Los Angeles usually has at most two of the three, which is the real reason storms stay rare near the beach and routine over the mountains.
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Every lightning bolt, rare or routine, follows the same physical sequence: ice collisions separate charge, a stepped leader gropes toward the ground, and a return stroke fires the flash you actually see.
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A hailstone is built inside a thunderstorm's updraft through repeated passes past supercooled water, not formed while falling. Southern California sees mostly small hail, concentrated over the mountains and deserts in summer.
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Fair-weather cumulus and a full cumulonimbus thunderstorm are the same cloud family at different stages of vertical growth. Watching how a tower changes shape over a few minutes reveals which one you are looking at.
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The saucer-shaped clouds that sometimes cap the San Gabriel Mountains aren't drifting, they're marking a fixed point in a standing wave of stable air flowing over the ridge.
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Southern California sees waterspouts most cool seasons, and nearly all of them are the weaker fair-weather type. The rarer tornadic kind can move onshore and become a genuine hazard.
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Over the Coachella Valley and Mojave Desert, rain often falls visibly from a cloud and vanishes before it ever reaches the sand. Here is why virga forms, and when the evaporating streaks turn into sudden desert wind gusts.
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From rare lowland snow and mountain snowpack to Death Valley heat, tornadoes, and the wind shear that challenges LA-area airports.
Downtown Los Angeles sees essentially no measurable snow, but the San Gabriel Mountains an hour away regularly get buried by the same winter storms. Elevation and freezing level explain the split.
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The Sierra Nevada snowpack works like a frozen reservoir, holding winter precipitation as snow and releasing it as spring and summer meltwater that reaches Southern California through the State Water Project and a wider supply network.
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Sleet, hail, and graupel are three different kinds of ice with three different flight paths through a storm cloud. Southern California mountain weather mostly delivers graupel, occasionally hail, and only rarely true sleet.
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Death Valley routinely tops 120°F in summer because of a rare combination of below-sea-level elevation, surrounding mountains, and bone-dry air. That same combination produced the hottest air temperature ever reliably recorded on Earth.
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Some Los Angeles neighborhoods stay noticeably warmer after sunset than nearby areas because pavement and buildings store daytime heat and release it slowly overnight.
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Tornadoes do hit Southern California, though they are far less frequent and usually far briefer than the classic Plains tornado. The official record shows confirmed events across the LA Basin and coast.
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A microburst is a small, violent thunderstorm downdraft that fans out in straight-line wind rather than rotating like a tornado. Southern California sees them most in summer desert storms.
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Wind shear is a sudden change in wind speed or direction that matters most during takeoff and landing. Sea-breeze fronts, mountain terrain, Santa Ana events, and thunderstorm outflow all produce it around Los Angeles airports.
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Strong wind lifts loose desert soil across the Coachella and Mojave deserts fast enough to turn a clear highway into a zero-visibility hazard in minutes. Here is how these storms form and what to check before you drive through one.
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The coast and the LA Basin get rain from the same storms that bury the San Bernardino, San Gabriel, and San Jacinto Mountains in snow. The dividing line sits around 5,000 to 6,500 feet, and it shifts with every storm.
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Unlike the LA lowlands or Palm Springs, Big Bear Lake genuinely gets snow most winters. But the town sits in a valley below the surrounding peaks, so storm totals, snowpack, and road conditions swing more between the lake and the ridgelines than most visitors expect.
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Pasadena and Mount Wilson can experience completely different winters during the exact same storm. The city stays wet and green at under 1,000 feet, while the peak looming over it, nearly 4,800 feet higher, is one of the most reliable snow views in the San Gabriels.
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The Palm Springs desert floor almost never sees snow, but the Aerial Tramway climbs nearly 6,000 vertical feet to reliable San Jacinto snowpack in about ten minutes, one of the sharpest winter elevation contrasts in the country.
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Los Angeles does not share one "hottest month": the coast typically peaks in late summer while inland valleys peak closer to July, a split driven by how slowly the Pacific Ocean warms.
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LA heat waves are not random hot days. They form when a stubborn high-pressure ridge sinks and dries the air overhead, shuts off marine cooling, and lets heat build for days in a row.
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The heat index estimates how hot LA air feels once humidity slows sweat evaporation, but it assumes shade and light wind. A humid coastal afternoon can carry a higher heat index than a hotter, drier inland one.
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Wet-bulb temperature measures how much cooling evaporation can still provide once you factor in humidity, not just how hot the air reads on a thermometer. Here is how it works and when it matters most in Southern California.
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A cool, overcast morning in Los Angeles can carry nearly as much sunburn risk as a hot, clear afternoon, because the UV Index tracks sun angle and elevation, not temperature or brightness.
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High surf, king tides, coastal erosion, tsunami risk, and the rare green flash that appears over the Southern California coast at sunset.
The Pacific off Los Angeles never averages 70°F in any month. This guide lists the monthly numbers from NOAA's Santa Monica Pier gauge, the best weeks to swim, and why the water can drop 7 degrees overnight.
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Long-period swell generated by storms far out in the Pacific can arrive on Los Angeles County beaches days later and under sunny skies. Wave period, direction, tide, and shoreline shape determine which beaches turn dangerous first.
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King tides are the highest predicted astronomical tides of the year, a calendar-driven preview of where sea level could sit on an ordinary day decades from now.
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Southern California beaches and bluffs retreat when wave energy, winter storms, sea level, and a sediment supply cut off by dams and development remove material faster than it returns.
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Southern California has recorded tsunami waves from both distant Pacific earthquakes and local offshore faults. Knowing the difference determines how much warning time you actually get.
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For a second or two at sunset, a clear Pacific horizon can turn the last sliver of the Sun bright green. It is real atmospheric refraction, not a myth or a camera trick.
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Malibu's south-facing points, coves, and cliffs bend and focus incoming swell instead of spreading it out evenly, so the same offshore storm can leave one beach calm and another genuinely dangerous a mile away.
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Rip currents are narrow channels of water racing away from shore through gaps in sandbars, not an undertow pulling swimmers under. Here is how to spot the channel and swim out of one safely.
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A sneaker wave is the one wave in an otherwise ordinary set that runs unusually far up the beach, catching people on dry sand rather than in the surf. Here is how it forms and where Southern California visitors are most exposed.
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Rogue waves are open-ocean events defined by how they compare to the surrounding sea state, not a label for any dramatic wave video. Here is how they form and how they differ from the shoreline hazards Southern California beachgoers actually face.
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The same Southern California algae bloom can tint the surf reddish-brown in daylight and make breaking waves glow electric blue after dark, two different effects from one organism.
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Month-by-month weather, the best times to visit, and what to pack for Los Angeles and nearby getaways, from the beach to the mountains and desert.
An August day in Woodland Hills swings about 37 degrees from night to afternoon, while Santa Monica changes about 13. This guide covers what to pack for Los Angeles month by month, plus extra gear for mountain, desert and stadium trips.
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Palm Springs has a sunny 70°F winter and a summer where 100°F afternoons are normal and nights stay near 80°F. This guide covers monthly temperatures, the best months to visit and the facts about summer heat.
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Big Bear Lake averages 46°F highs and 24°F lows in January and about 80°F by day and 50°F at night in July, with about 59 inches of snow a season. This guide covers each month and the conditions LA visitors most often underestimate.
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Santa Monica stays between about 66°F and 77°F all year, yet a June beach day often starts under gray cloud and the water is only warm from late July to early October. This guide covers each month.
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Avalon averages about 63°F in winter and 75°F in August, while the ridge-top airport is warmer in summer and often foggy in spring. This guide covers Catalina month by month, plus when the crossing is roughest and the water warmest.
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A month-by-month guide to Los Angeles weather with beach, Downtown and Valley temperatures side by side, rain, ocean temperature and the patterns that surprise visitors.
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October is warmer than June in Downtown Los Angeles, and nearly every October brings a 90-degree day. This guide covers what to expect, from Santa Ana winds to the first storm of the season.
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Record heat, record cold, and the storms and floods that shaped Los Angeles, told with the station data behind them.
Downtown Los Angeles last hit 32°F on January 29, 1979. Its record, 28°F, was set in 1883 and tied in 1913 and 1949, and Woodland Hills holds the city low of 18°F. This guide covers LA's cold records and why frost is disappearing.
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Rain fell on Los Angeles from December 24, 1861 to January 23, 1862 with only two breaks. The flood swept away the city's water works, moved the San Gabriel River and nearly erased Agua Mansa. This guide covers what happened in Los Angeles and when a flood like it could return.
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Downtown Los Angeles hit 113°F on September 27, 2010, just before its sensor failed. Woodland Hills reached 121°F in 2020. This guide lists LA's heat records, station by station, and explains why most fall in September.
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The 1997-98 El Niño doubled Los Angeles rainfall and gave LA its wettest February on record. With the Pacific running even warmer in 2026, this guide covers what happened and what LA history says about this winter.
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Game-day, event and outing weather for LA stadiums, parades, parks and airports: what to expect, what to wear, and what to check before you go.
Around 6 a.m., LAX sits under low clouds or poor visibility nearly one hour in five; by 2 p.m., one hour in thirty. This guide covers when the marine layer, east winds and storms slow flights, and how to check before you go.
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Gray whales migrate past Los Angeles in winter, when waves average 4 to 5 feet offshore. Blue whales feed in summer, when seas drop to about 3 feet. This guide shows how to pick a season, a time of day and a forecast.
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Rain has hit the Rose Parade about a dozen times, most recently in 2026. This guide covers how often New Year's Day is wet, how cold a Pasadena parade morning gets, and what to pack for the curb.
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SoFi has a fixed, translucent roof and no walls. This guide explains what that means for rain, wind and temperature, from a 78°F September kickoff to a 58°F December fourth quarter.
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A typical Dodgers night game starts near 65°F in April and 75°F in August, then cools several degrees by the late innings. This guide covers game-time weather by month, where the shade falls, and what to bring.
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