Canadian drought monitor
North American drought monitor
https://droughtmonitor.unl.edu/nadm/Home.aspx
Global drought monitor
https://gdis-noaa.hub.arcgis.com/pages/drought-monitoring
Copernicus global drought monitor
https://drought.emergency.copernicus.eu/
Spei global drought monitor
https://spei.csic.es/map/maps.html#months=1#month=7#year=2026
Link to Google search
https://share.google/aimode/hj07eLtPVJiF5BnyI
Water levels at Lyman Lake in Arizona are currently low, sitting around 31 feet below full pool (approximately 5,948.70 feet surface elevation), according to live data from Lakebrief. [1]
Current Conditions & Status
- Boat Ramps: All boat ramps at Lyman Lake State Park are closed until water levels rise to a safe standard.
- Park Amenities: Restrooms and showers are fully functional, but there is no drinking water available at the park.
- Water Temperature: Approximately 67°F.
- General Cause: Low levels are driven by long-term regional dry conditions, low snowpack, and limited monsoon inflow. [2, 3, 4]
If you are planning a trip, would you like information on alternative nearby lakes for boating or shoreline camping options currently available at the park?
No, recent rainfall has not provided any meaningful improvement. While live USGS data indicates a very minor 7-day upward tick of less than half a foot (+0.43 ft), the lake remains critically low at only 6% of its total capacity. [1]
Because the lake is roughly 31 feet below its full pool level, a slight increase from localized rain is not nearly enough to change conditions. The Arizona State Park system maintains that all motorized boat ramps remain completely closeduntil a sustained, substantial rise in water levels occurs. Furthermore, a Harmful Algal Bloom (HAB) warning remains active for the lake due to the stagnant, low-water conditions. [1, 2]
Would you like to explore other recreational activities at Lyman Lake that don't depend on the water level, such as hiking the Peninsula Petroglyph Trail, or would you like to know about nearby bodies of water that currently allow motorized boats?
Yes, the monsoon season is officially over. In Arizona, the National Weather Service sets strict, fixed dates for the monsoon season, which runs from June 15 through September 30 each year. [1]
Because yesterday marked the final day of the season, regional weather patterns are shifting away from the southern tropical moisture flows that trigger severe afternoon thunderstorms. The forecast for the Lyman Lake area is transitioning into a much drier, calmer autumn pattern. [2, 3, 4]
- No Seasonal Relief: Since the monsoon season has wrapped up without delivering significant rain to the Apache County region, there is no further chance of summer storms replenishing the lake. [2]
- Next Water Inflow: Any meaningful rise in Lyman Lake's water levels will now depend entirely on winter snowpack in the surrounding mountains and subsequent spring runoff. [5, 6]
Are you trying to figure out when the lake conditions might improve, or would you like to explore other high-country lakes in Arizona that weren't as heavily impacted by the dry summer?
[1] https://energy.ecoflow.com
Yes, Canada has a direct equivalent called the Canadian Drought Monitor (CDM). [1]
Managed by Agriculture and Agri-Food Canada (AAFC), the system was established in 2002. It is explicitly designed using the exact same science, methodology, and visual styling as the highly successful United States Drought Monitor. [1]
- The Same 5-Category Scale: Just like the U.S. version, Canada classifies dry conditions using five distinct tiers:
- D0: Abnormally Dry
- D1: Moderate Drought
- D2: Severe Drought
- D3: Extreme Drought
- D4: Exceptional Drought [2]
- Unified Continental View: Because they use the exact same metrics, Canada, the U.S., and Mexico pool their monthly assessments together to build the North American Drought Monitor (NADM), providing a seamless, border-to-border view of continental drought conditions. [3]
- Data Synthesis: The CDM blends multiple complex variables into its monthly maps—including temperature records, precipitation data, streamflow, soil moisture levels, and localized impact assessments from forestry and agricultural sectors. [4, 5]
The primary difference is the update frequency. While the U.S. Drought Monitor updates weekly, the official Canadian Drought Monitor releases map assessments once per month (usually around the 10th day of the month to reflect the previous month's final data). [6]
If you want to track a particular area, let me know:
- What specific province or region in Canada are you interested in?
- Are you looking for real-time agricultural impacts or long-term water supply forecasts?
I can guide you to regional tools, like Alberta's AgroClimatic Service, which provide more localized weekly updates. [7]
[1] https://agriculture.canada.ca
[2] https://www.theweathernetwork.com
[4] https://agriculture.canada.ca
That is a completely fair point. The landing pages require clicking through multiple sub-menus to actually find the visual files.
Direct links to the actual map viewing pages and download applications include:
🇨🇦 Canadian Drought Monitor Maps
- Interactive Map Viewer: To explore current regional conditions with full interactive map controls, use the Canadian Drought Monitor Current Conditions Viewer.
- Static Maps & PDF Archives: If you prefer viewing or downloading high-quality monthly static maps, you can access the compiled list directly on Agriculture and Agri-Food Canada's Map Archive.
🌎 North American Drought Monitor Maps
- Continental Map Application: The official continental map displaying Canada, the U.S., and Mexico seamlessly together can be viewed directly on the UNL North American Drought Monitor Map Portal.
- Multilingual Map Downloads: If you are looking for specific monthly historical maps, the NOAA interface allows you to select the exact month and year to download via the NCEI NADM Map Repository.
Yes, there are several highly advanced worldwide drought monitors. Because tracking drought globally requires immense satellite processing, the international scientific community handles it using two different strategies: a "bottom-up" approach that stitches regional national maps together, and a "top-down" approach that uses global satellite telemetry. [1]
The primary global platforms with direct access to interactive maps include:
1. Global Drought Information System (GDIS)
The GDIS Portal uses a "bottom-up" philosophy. It pulls the official data created by individual nations (like the U.S. and Canadian Drought Monitors) and merges them into a single interface. [1]
- Interactive Tool: You can zoom in on any continent using the GDIS Interactive Global Drought Monitor to see how local assessments stitch together across borders. [1]
2. Copernicus Global Drought Observatory (GDO)
Run by the European Commission, the GDO relies on pure satellite observation and climate modeling. It monitors the entire planet's precipitation anomalies, soil moisture levels, and vegetation health. [2, 3]
- Interactive Tool: The Copernicus GDO MapViewer allows you to toggling multiple global layers, including ground-water availability and agricultural drought risks. [2, 4]
3. SPEI Global Drought Monitor
For climatologists who look strictly at the math of water evaporation, the Spanish National Research Council hosts a dedicated scientific platform. It tracks the Standardized Precipitation Evapotranspiration Index (SPEI) at a global scale.[5, 6]
- Interactive Tool: You can manipulate the time-scale from a short 1-month window up to a massive 48-month structural tracking window on the SPEI Global Map Interface.
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It is entirely natural to look at these global trends with concern. Large-scale shifts in weather patterns have made intense, prolonged droughts increasingly visible on every continent.
If you want a quick, macro-level snapshot of what these global monitors are currently showing, here are the three major regions experiencing the most severe structural drought stress right now:
- Southern Africa: Driven by a powerful combination of consecutive dry seasons and changing climate patterns, large portions of Zambia, Zimbabwe, and Malawi are facing critical water scarcity and agricultural strain.
- The Amazon Basin: The world's largest rainforest has been enduring historic low water levels in its river systems, impacting local transportation, biodiversity, and regional moisture cycles.
- Parts of Southern & Eastern Europe: While northern regions have seen plenty of rain, the Mediterranean basin and areas around southeastern Europe continue to experience long-term groundwater deficits.
Because global weather is highly volatile, would you like me to set up a task to check back in a few months and provide you with an updated summary of how these global drought zones are shifting as we enter the next season?
you looking to use these maps for a general global overview, or do you have a specific country outside of North America (such as a country in Europe or Africa) whose local tracking system you want to find?
[1] https://gdis-noaa.hub.arcgis.com
[2] https://joint-research-centre.ec.europa.eu
The current historic "Super" El Niño event is expected to severely worsen droughts across Southern Africa and the Amazon Basin, while having a more complex, indirect impact on Southern Europe. [1, 2]
Meteorologists at NOAA's Climate Prediction Center have verified a 75% chance that the late 2026 Oceanic Niño Index will break all-time records dating back to 1950. When El Niño reaches this "super" magnitude, it aggressively alters global atmospheric circulation, shifting rainfall away from traditional tropical zones. [3, 4, 5, 6]
Here is how this massive climate event is projected to impact each of those three specific regions:
1. Southern Africa: Catastrophic Drying Ahead
- The Mechanism: El Niño alters the African jet stream, effectively blocking moisture from moving inward from the Indian Ocean.
- The Impact: For countries like Zambia, Zimbabwe, and South Africa, El Niño is historically the single most consistent driver of severe agricultural drought. Because this event is tracking at record-breaking speeds, experts warn it will trigger widespread crop failures and acute livestock water shortages through the peak 2026–2027 growing season. [2, 7, 8, 9]
2. The Amazon Basin: Record Lows and Extreme Fire Risk
- The Mechanism: The immense warming in the Pacific shifts rising air currents eastward. This creates a powerful zone of sinking, dry air directly over northern South America, choking off the basin's rainfall. [5]
- The Impact: The Amazon is already structurally vulnerable from previous dry seasons. The World Resources Institute notes that this Super El Niño will suppress vital rains well into 2027, severely lowering the Amazon River's water levels further and skyrocketing the risk of catastrophic forest fires. [1, 8]
3. Southern & Eastern Europe: Indirect, Variable Effects
- The Mechanism: Unlike the tropics, Europe does not have a direct physical link to Pacific sea temperatures. Instead, El Niño acts like a row of falling dominoes, nudging the Atlantic jet stream and altering how winter storm tracks approach the continent. [5]
- The Impact: El Niño will not automatically dictate a drought here. Instead, the global baseline warming trend combined with El Niño's disruption to the polar vortex creates highly volatile weather. Southern and Eastern Europe face a dual threat: localized shifts can trigger sudden, intense summer heatwaves that dry out soil rapidly, even if the winter brings sporadic rain. [2, 5, 10]
Would you like to look at how this Super El Niño is expected to impact your local weather in the United States this winter, or would you like to see which global regions are actually expected to get flooding rains (such as East Africa or Peru) instead of drought?
[3] https://www.cpc.ncep.noaa.gov
[4] https://wmo.int
[5] https://blog.plant-for-the-planet.org
[8] https://www.theclimatebrink.com
[10] https://salatainstitute.harvard.edu
The historic 2026 "Super" El Niño is expected to bring substantial drought relief to the Southwest, while simultaneously worsening drought conditions across the Pacific Northwest. Because this NOAA Climate Prediction Center event is tracking to be potentially the strongest in recorded history, its ability to alter weather patterns across the American West is highly pronounced, splitting the region into two starkly different climate zones. [1, 2, 3]
- Above-Average Rain & Snow: A strong El Niño intensifies and shifts the subtropical jet stream further south. This regularly steers atmospheric rivers and heavy winter storms directly across California, Arizona, Nevada, Utah, and New Mexico. [2]
- Reservoir Recharge: According to the USGS Climate Adaptation Science Centers, this pattern significantly increases the likelihood of a deep winter snowpack in the Sierra Nevada and southern Rockies. This runoff is critical for recharging major water systems and replenishing drought-depleted reservoirs like Lake Mead and Lake Powell. [2, 4]
- Warmer & Drier Conditions: Conversely, northern states like Washington, Oregon, Idaho, and western Montana are typically bypassed by these southern storm tracks during an El Niño of this magnitude. [1, 5]
- Snowpack Deficits: The USDA Northwest Climate Hub warns that warmer winter temperatures will cause more precipitation to fall as rain rather than snow. This causes lower mountain snowpack, reduced spring runoff, and an elevated risk of During a "Super" El Niño, the Northeast experiences a distinct divide because the climate pattern pushes a moisture-rich southern jet stream up the East Coast. This sets up a battle between coastal tropical air and colder northern air. [1, 2, 3]
Because of their geographical positions, Westchester County, NY and Coös County, NH face completely opposite outcomes regarding drought and winter precipitation:
🗽 Westchester County, NY: Widespread Drought Relief
- The Outlook: Significant drought improvement or complete removal.
- The Pattern: Westchester sits directly in the crosshairs of the coastal storm track. Super El Niño conditions heavily favor the development of frequent, powerful nor'easters pumping moisture straight from the Atlantic. [1, 4]
- Rain vs. Snow: Because El Niño also brings a general baseline of warmer, milder winter temperatures along the I-95 corridor, Westchester's winter will likely feature a lot of heavy rain, freezing sleet, and dense, slushy snow rather than light powder. While it might make for a messy winter, the constant influx of heavy precipitation will thoroughly recharge local groundwater and reservoirs. [2, 3, 5, 6, 7]
🏔️ Coös County, NH: At Risk for Persisting Dryness
- The Outlook: Drought conditions may persist or worsen.
- The Pattern: As the northernmost county in New Hampshire, Coös County sits too far inland and north to reliably catch the moisture from these southern-tracked nor'easters. During strong El Niños, the northern tier of the United States typically experiences drier-than-average and warmer-than-average winter conditions. [4, 8, 9, 10]
- Snowpack Deficits: The Northeast Regional Climate Center notes that interior New England historically sees below-average winter snowfall during strong El Niño events. Without a deep winter snowpack, Coös County could see reduced spring runoff, potentially exacerbating structural or agricultural drought heading into 2027. [9, 11]
Are you monitoring these counties for agricultural purposes (like soil health or farming), or are you tracking winter recreation conditions (such as ski resort snowpack in the White Mountains)?
[1] https://www.nbcnewyork.com
[4] https://elnino.nrcc.cornell.edu
[5] https://www.northjersey.com
[9] https://elnino.nrcc.cornell.edu
[10] https://weather.com
[11] https://www.wtnh.com
- prolonged structural drought into 2027. [1]
Would you like to check the specific winter precipitation forecast for your exact state or city, or would you like to see the current U.S. Drought Monitor map for the Western region?
[1] https://www.climatehubs.usda.gov
Both regions currently face elevated fire danger due to prolonged dry conditions, though their active restrictions and immediate outlooks differ significantly.
Because a regional drought remains widespread across the Northeast, local vegetation has dried out into highly flammable fuel. [1]
🗽 Westchester County, NY: Burn Ban Implemented
- Current Fire Danger: High. The continued lack of rain and persistent winds have rapidly dried out the ground fuels. [2, 3]
- Active Restrictions: A temporary statewide burn ban is actively in effect to curb wildfire risks. Starting outdoor fires for brush or debris disposal, as well as all uncontained campfires and open fires, is strictly prohibited. [2]
- El Niño Context: While the upcoming Super El Niño favors drought-busting rain and storms later this winter, the immediate autumn window remains highly vulnerable until those heavy precipitation tracks firmly establish.
🏔️ Coös County, NH: High Risk with Strict Bans
- Current Fire Danger: Very High to Severe. The interior of New England has borne the brunt of the dry summer, leaving forests primed for rapid wildfire ignition and spread. [4, 5]
- Active Restrictions: An emergency statewide burn ban remains active under executive order. All open fires—including backyard fire pits, campfires, and lawn debris burning—are banned. Furthermore, smoking near woodlands or on public trails is entirely prohibited, and all state-issued burn permits are suspended until further notice. [4]
- El Niño Context: Because Coös County faces a higher likelihood of a warmer, drier winter with a below-average snowpack due to the El Niño pattern, this fire risk may take much longer to naturally subside compared to coastal areas.
Before doing any outdoor activities, you can check daily local condition shifts via the New York State DEC Fire Danger Map or the New Hampshire Division of Forests and Lands Portal.
[1] https://www.weatherbug.com
[2] https://www.newrochelleny.gov
[4] https://hollisbrooklinenews.org
You are completely correct: climate change is making the Northeast significantly wetter overall. In fact, data from the U.S. National Climate Assessment confirms that the Northeast has seen a 60% increase in extreme precipitation events over recent decades—the largest regional jump anywhere in the United States. [1]
However, a landmark study from Dartmouth College outlines a paradox in how this water is delivered, which explains why the region is currently experiencing acute fire danger and flash droughts: [2]
1. The "Tug-of-War" Dynamics
As temperatures warm, the atmosphere holds more moisture (roughly 7% more per degree Celsius), but it also accelerates evapotranspiration—the rate at which water evaporates out of plants and soil. Right now, the Northeast is experiencing a temporary "tug-of-war" where extreme, short-term heat spikes dry out the landscape faster than the rain can replenish it.[3, 4]
2. Consolidated Rain, Longer Dry Spells
Climate change isn't making it rain gently or consistently throughout the year. Instead, research shows that rainfall is consolidating into shorter, much more violent bursts, leaving longer stretches of completely dry days in between. [5]
- The Result: When a month's worth of rain drops in a single afternoon, it creates massive runoff and flash flooding rather than soaking deeply into the water table. Once that storm passes, a multi-week dry spell combined with high autumn winds can instantly turn the top layer of brush into a wildfire hazard, creating the high fire danger despite the broader "wetter" climate trend. [3, 6]
3. Fewer Long-Term Structural Droughts
The good news from the Dartmouth study is that because total annual rainfall has risen, the massive, multi-year structural droughts that used to dry up the Northeast's reservoirs are 59% less frequent than they were in the 20th century. [2]
So while the region is getting wetter on a macro scale, the day-to-day reality alternates wildly between sudden deluges and sudden fire risks. [6, 7]
Would you like to know more about how your local community is updating infrastructure to handle these extreme 4-to-5-inch rain events, or are you interested in tracking when the next atmospheric river is projected to hit the East Coast?
[2] https://home.dartmouth.edu
[4] https://x.com
[7] https://www.eurekalert.org
Another Google link
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