Plaincast decodes the National Weather Service's Area Forecast Discussion — the real forecast, written 3 to 4 times a day by the meteorologist on shift — into plain English. The discussion is where a forecaster explains their reasoning: which models disagree, what they are watching, and how confident they are. Below is the current edition for Miami, with its shorthand expanded. The full experience — an AI plain-English summary beside the annotated original — loads with JavaScript, and every one of the 68 forecast offices has its own edition.
Area Forecast Discussion · National Weather Service Miami (MFL) · issued Friday, September 11 at 7:27 AM EDT.
Messages
Numerous showers and thunderstorms are forecast today, focusing along the east coast this morning before the bulk of activity shifts over southwestern Florida in the PM. Gusty winds and dangerous cloud to ground lightning is possible with any storm.
A moderate risk of rip currents is forecast at Palm Beach County beaches today.
High temperatures will generally rise into the low to mid 90s across South Florida through the upcoming weekend, resulting in widespread Moderate to Major HeatRisk each day.
Short Term
(Today through Saturday) Issued at 233 AM EDT Fri Sep 11 2026
We have noticed a few key features from looking over visible satellite imagery yesterday afternoon. Widespread anvil debris from antecedent thunderstorm activity across much of South Florida is one of them, with the second being a residual outflow boundary (a direct byproduct of t-storm activity that formed outside of Biscayne Bay and pushed through the east coast metro) that has remained practically stationary across our nearshore Atlantic waters. This upper-level cloud cover has resulted in not only cooler temperatures across our east coast observing sites (some stations such as KMIA may have actually already recorded their low temperature yesterday afternoon after being enveloped in this rain-cooled environment) but the formation of a land breeze across our immediate east coast which, for the time being, has allowed individualized showers that have fired up along the aforementioned outflow boundary to stay over our local Atlantic waters. With the prevailing surface flow being out of the east, however, we can anticipate these showers to continue inching closer to the east coast through these early morning hours before eventually falling apart shortly upon moving onshore due to the loss of best nighttime environmental dynamics over the water and the rather stable boundary layer over mainland South Florida. Mesoanalysis indicates that this lingering outflow boundary will not be persisting over the local waters for much longer, but will continue to act as a short-fuse focus of ascent before easterly flow reestablishes itself and erodes it through daybreak. In addition to this, mid-level water vapor imagery shows plenty of moisture residing around the Lake Okeechobee region and SW Florida in response to a 500-mb perturbation that has been, and still is, lifting through our region since yesterday (and what evidently prompted shower and thunderstorm activity, through amplified forcing aloft, to be a little more widespread in nature). The passage of this upper-level disturbance is not only being noted on mesoanalysis but also on regional ACARS soundings as a localized enhancement and erratic shifts in wind speeds at and around that specific pressure height.
The aforementioned impulse will be ejected to our north and exiting our vicinity as the rest of the day progresses as it rides the western periphery of a mid-level subtropical ridge towards central Florida and eventually into the nearshore Atlantic waters of the Southeast United States, attempting to merge with another shortwave feature crossing the AL/GA region zonally thereafter. At the surface, as previously mentioned, an easterly flow regime is expected to prevail across South Florida at the expense of expansive surface ridging over the subtropical Atlantic. Although we will be losing the primary forcing mechanism aloft with the departure of our mid-level disturbance, anomalously high precipitable water, as per HREF guidance, between the 70th and 90th percentiles (equating to 2.0-2.2") combined with ample surface-based instability (3500-4500 J/Kg) building throughout the daily cycle should be sufficient to support scattered showers and thunderstorms across mainland South Florida once again. LPMM composite reflectivity shows cells initially firing up during the morning hours along the east coast sea breeze and subsequently becoming more numerous in nature as they push inland towards the interior and SW Florida during the afternoon hours. Rather unimpressive localized dynamics (poor low to mid level lapse rates, warm 500mb temperatures falling within the 50th to 75th percentiles for the date, and weak background flow) should keep the threat of storms reaching strong to severe thresholds low. The atmosphere has been conducive enough over the past few days to pump out sub-SPS wind gusts of anywhere between 20 and 40 mph, and with a similar environment today, should continue to be a potential hazard to be aware of. Heavy rainfall, localized flooding (especially around our Gulf coast locales with the diurnally-induced Gulf sea breeze looking to counteract our prevailing easterly flow) and frequent/dangerous lightning strikes should be the other risks we will have to contend with. HREF shows neighboring probs of 10-30% of rainfall rates exceeding an inch per hour along this pinned Gulf sea breeze.
Rinse and repeat on Saturday, although there will be a few minor, and we really mean minor, changes to the upper-level pattern. Surface ridging will remain in place across the subtropical Atlantic, keeping our easterly flow set in stone. Barely aloft at around the 850-mb height level, a weak impulse which will be located around eastern Cuba on Friday will be steadily riding the southwestern periphery of another coinciding ridge at the same isobaric height and reaching our general vicinity to kick off the weekend. This, according to the National Blend of Models (the blend-of-models forecast), will bring a modest moisture surge to our region along with some coincident forcing. precipitable water are forecast to rise ever so slightly to the 2.1-2.3" range and, in addition to the introduction of the aforementioned shortwave, will result in a corresponding uptick in regional chance of rain to around the 70-90% range, up from 60-80% on Friday. Routine summertime pattern in the sense that showers and storms will be residing over the local waters (and briefly pushing onshore) during the overnight hours when and where cyclical instability will be highest, followed by an increase in such activity over the mainland during the afternoon period. With easterly flow, convection will look to once again favor the western half of South Florida during peak heating of the day. Though with a slightly veering flow in the lowest 3 km of the atmosphere from southeasterly today to southerly on Saturday due to a small westward shift in our low to mid level subtropical ridge, it is possible we get the interior and eastern metros more involved than Friday with the elevated amounts of moisture and forcing simply bolstering a higher coverage of overall storms. With a fairly similar mesoscale setup expected with respect to our prevailing easterly flow and emerging Gulf sea breeze, these counteracting features could present a localized flood risk from nearly stationary/boundary-derived cells over surrounding areas. Forecast soundings and overall unamusing dynamics suggest the severe threat will once again be minuscule, with gusty and erratic winds, frequent lightning, and indubitably heavy downpours being the main hazards in and around the strongest thunderstorms.
High temperatures will look to climb into the low to mid 90s both today and Saturday with max apparent temperatures generally in the 100-105F range. Wherever convection fails to traverse early in the day along our coastal metro areas is where the heat will be able to build quickest after daybreak. However, look for more widespread relief later in the day as both showers/thunderstorms and upper-level cloud canopies increase in areal coverage.