Summer monsoon rain over eastern New Mexico

The North American monsoon, variously known as the Southwest monsoon, the Mexican monsoon, the New Mexican monsoon, or the Arizona monsoon[1] is a pattern of pronounced increase in thunderstorms and rainfall over large areas of the southwestern United States and northwestern Mexico, centered roughly on the Rio Grande Valley, and typically occurring between June and mid-September. During the monsoon, thunderstorms are fueled by daytime heating and build up during the late afternoon and early evening. Typically, these storms dissipate by late night, and the next day starts out fair, with the cycle repeating daily. The monsoon typically loses its energy by mid-September when much drier conditions are reestablished over the region. Geographically, the North American monsoon precipitation region is centered over the Sierra Madre Occidental in the Mexican states of Sinaloa, Durango, Sonora and Chihuahua.[2]

Mechanism

Weather pattern of the North American monsoon
Typical precipitation pattern of the North American monsoon (green arrow)

The North American monsoon is a complex weather process that brings moisture from the Gulf of California (and to lesser extent the eastern Pacific and Gulf of Mexico) over northwestern Mexico and southwestern US resulting in summer thunderstorms, especially at higher elevations. The North American monsoon is not as strong or persistent as its Indian counterpart, mainly because the Mexican Plateau is not as high or as large as the Tibetan Plateau in Asia. However, the North American monsoon shares most of the basic characteristics of its Indian counterpart.[3]

In the monsoon area, the late spring period is very hot and dry, because the dry western side subtropical high pressure ridge and dry continental air have not begun to 'shift' northwards yet. During this period, inland areas have extremely low relative humidity, and characteristically very low dew points, which are frequently well below the freezing mark. In some years, this delayed effect is more substantial if the dryline which separates the hot and dry airmass to the Northwest from the humid monsoon airmass to the Southeast, fails to migrate. This can prevent tropical moisture from reaching farther Northwest towards Death Valley until later in the summer. If this pattern prevails, the Nevada deserts may receive almost no monsoon.

In early summer, the monsoon starts with a shift in wind patterns as Mexico and the southwest U.S. warm under intense solar heating.[4] The prevailing winds start to flow from somewhat cooler moist ocean areas into hotter, dry land areas.[3] Precipitation increases in late May to early June in southern Mexico and spreads along the western slopes of the Sierra Madre Occidental, reaching New Mexico and southeast Arizona and in early July. It extends into the southwest United States as it matures in mid-July, when an area of high pressure, called the monsoon or subtropical ridge, develops in the upper atmosphere over the Four Corners region, creating wind flow aloft from the east or southeast.[5] At the same time, a thermal low (a trough of low pressure from intense surface heating) develops over the Mexican Plateau and the Desert Southwest of the United States.[6]

The thermal low sets up circulation that brings pulses of low level moisture from the Gulf of California and eastern Pacific. The Gulf of California, a narrow body of water surrounded by mountains, is particularly important for low-level moisture transport into Arizona and Sonora. Upper level moisture is also transported into the region, mainly from the Gulf of Mexico by easterly winds aloft. Once the forests of the Sierra Madre Occidental green up from the initial monsoon rains, evaporation and plant transpiration can add additional moisture to the atmosphere which will then flow into Arizona and New Mexico. Finally, if the southern Plains of the U.S. are unusually wet and green during the early summer months, that area can also serve as a moisture source.[3]

As precipitable water values rise in early summer, brief but often torrential thunderstorms can occur, especially over mountainous terrain.[7] This activity is occasionally enhanced by the passage of tropical waves and the entrainment of the remnants of tropical cyclones.[8][9]

Effects

A seasonal monsoon storm approaching the Tiger Fire on July 9, 2021

Monsoon precipitation accounts for a substantial portion of annual precipitation in northwest Mexico and the Southwest U.S. Most of these areas receive over half their annual precipitation from the monsoon.[3] Many desert plants are adapted to take advantage of this brief wet season. Because of the monsoons, the Sonoran and Mojave are considered relatively "wet" when ranked among other deserts such as the Sahara, and helps fuel the Chihuahuan Desert's extreme diversity.

Monsoons often play a role in reducing wildfire threat by providing moisture at higher elevations during the wildfire season.[10] Heavy monsoon rain can lead to excess winter plant growth, in turn a summer wildfire risk. A lack of monsoon rain can hamper summer seeding, reducing excess winter plant growth but worsening drought.

Flash flooding is a serious danger during the monsoon. Dry washes can become raging rivers in an instant, even when no storms are visible as a storm can cause a flash flood tens of miles away.[11] Lightning strikes are also a significant danger. Because it is dangerous to be caught in the open when these storms suddenly appear, many golf courses in Arizona have thunderstorm warning systems.

Once the monsoon is underway, mountain ranges, including the Sierra Madre Occidental, the Mogollon Rim, and the Rio Grande Rift ranges provide a focusing mechanism for the daily development of thunderstorms. Thus much of the monsoon rainfall occurs in mountainous terrain. For example, monsoon rainfall in the Sierra Madre Occidental typically ranges from 10 to 15 inches. Since the southwest U.S. is at the northern fringe of the monsoon, precipitation is less and tends to be more variable. Areas farther west of the core monsoon region, namely California and Baja California, typically receive only spotty monsoon-related rainfall. In those areas, the intense solar heating is not strong enough to overcome a continual supply of cold water from the North Pacific Ocean moving down the west coast of North America. Winds do turn toward the land in these areas, but the cool moist air actually stabilizes the atmosphere.[3] The monsoon pushes as far west as the Peninsular Ranges and Transverse Ranges of Southern California, but rarely reaches the coastal strip. As shown in the panorama below, a wall of thunderstorms, only a half-hour's drive away, is a common sight from the sunny skies along the coast during the monsoon.

Monsoonal thunderstorms as seen from El Cajon, California

Variability

An isolated thunderstorm rolls through Wah Wah Valley, Utah. This type of monsoonal pattern is very common in the late summer of the southwest US.

Rainfall during the monsoon is not continuous. It varies considerably, depending on a variety of factors. There are usually distinct "burst" periods of heavy rain during the monsoon, and "break" periods with little or no rain.[3] The variability is difficult to understand and predict, because it results from the complex interactions between atmospheric circulation features at both the synoptic (100 to 1000 km spatially, 1 day to 1 week, temporally) and mesoscale (several km to 100 km, hours to one day temporally) and the extremely varied topography. The larger-scale atmospheric motions may control the distribution of water vapor and the general stability or instability (that is, the tendency to form storms) in the atmosphere; nevertheless, local topographic effects are critical to the geographic and even temporal distribution of convective activity.[2]

The monsoon ridge is almost as strong as the one which develops over Asia during the summer. However, since the lower level moisture flow is not as persistent as in the Indian monsoon, the upper level steering pattern and disturbances around the ridge are critical for influencing where thunderstorms develop on any given day. The exact strength and position of the subtropical ridge also governs how far north the tropical easterly winds aloft can spread. If the ridge is too close to a particular area, the sinking air at its center suppresses thunderstorms and can result in a significant monsoon "break." If the ridge is too far away or too weak, the east winds around the high are inadequate to bring tropical moisture into the mountains of Mexico and southwest U.S. However, if the ridge sets up in a few key locations, widespread and potentially severe thunderstorms can develop.[3]

Monsoon variability from one summer to the next is substantial, and exceeds the normal monsoon seasonal precipitation at most locations. For example, the normal monsoon precipitation at Tucson, Arizona is 6.06 inches (154 mm). The driest monsoon season measured 1.59 inches (40 mm), and the wettest measured 13.84 inches (352 mm).[12]

Research since 2010 has investigated the possible causes behind North American monsoon variability. The following factors are affect the North American monsoon:

None of these factors can perfectly predict the variability. These factors are related to each other and are not independent. For example, sea surface temperatures affect all the other factors to some extent.[12]

In some years, the Nevada deserts may receive almost no monsoon influence if the western subtropical high shifts less than in typical years. For instance in 2020, the subtropical high remained further south than usual due to the influence of a strong ridge of high pressure over the northern Pacific, displacing the jet stream further inland.[5] The combination of these factors blocked moist tropical air from reaching the American Southwest, leading to below average rainfall.

Definition of monsoon

Whether the North American monsoon is a "true monsoon" has been controversial. Until the late 1970s, there was serious debate about whether a monsoon truly existed in North America. However, considerable research, which culminated in the Southwest Arizona Monsoon Project (SWAMP) in 1990 and 1993,[13][14] established the fact that a bonafide monsoon, characterized by large-scale wind and rainfall shifts in the summer, develops over much of Mexico and the intermountain region of the U.S.[3]

The controversy continues because of the incomplete reversal of the winds during the monsoon. The prevailing winds shift from westerly pre-monsoon to southerly during the monsoon.[4][15] Because this is not a complete 180-degree reversal, some climatologists claim the North American monsoon is not a true monsoon.[16] Other climatologists claim it is a real monsoon.[17]

See also

References

  1. ↑ Adams, David; Comrie, Andrew (1997). "The North American Monsoon". Bulletin of the American Meteorological Society. 78 (10): 2197–2213. Bibcode:1997BAMS...78.2197A. doi:10.1175/1520-0477(1997)078<2197:TNAM>2.0.CO;2.
  2. 1 2 Public Domain This article incorporates public domain material from Adams, David K. (1997). "Review of Variability in the North American Monsoon". Impact of Climate Change and Land Use in the Southwestern United States. United States Geological Survey.
  3. 1 2 3 4 5 6 7 8 Public Domain This article incorporates public domain material from North American Monsoon. National Weather Service. Archived from the original on June 12, 2008.
  4. 1 2 Grantz, K; Rajagopalan, B; Clark, M; Zagona, E (2007). "Seasonal Shifts in the North American Monsoon". Journal of Climate. 20 (9): 1923–1935. Bibcode:2007JCli...20.1923G. doi:10.1175/JCLI4091.1. S2CID 55111148. Retrieved September 14, 2022.
  5. 1 2 Duginski, Paul (August 9, 2020). "Drought continues to expand as the monsoon in the Southwest has been largely a no-show". Los Angeles Times. Retrieved June 16, 2021.
  6. ↑ "The Monsoon". National Weather Service Forecast Office Flagstaff, Arizona. Archived from the original on February 28, 2008. Retrieved February 28, 2008.
  7. ↑ Junker, Norman W. "Maddox Type IV Event". Retrieved February 29, 2008.
  8. ↑ "Reports to the Nation: The North American Monsoon" (PDF). Climate Prediction Center. Retrieved February 29, 2008.
  9. ↑ Roth, David M. "Tropical Cyclone Rainfall for the West". Retrieved February 29, 2008.
  10. ↑ US Crop Reporting Board, Bureau of Agricultural Economics, Agricultural Marketing Service, and Agricultural Statistics Board (2006). Crop Production. Crop Reporting Board, Statistical Reporting Service, U.S. Department of Agriculture. pp. 30, 36.{{cite book}}: CS1 maint: multiple names: authors list (link)
  11. ↑ "North American Monsoon Flash Floods". NOAA. Retrieved November 9, 2022.
  12. 1 2 Public Domain This article incorporates public domain material from Monsoon Inter-annual Variability (PDF). National Weather Service. Retrieved September 14, 2022.
  13. ↑ Reyes, S; Douglas, MW; Maddox, RA (1994). "El Monzon del suroeste de Norteamérica (TRAVASON/SWAMP)". Atmósfera. 7: 117–137.
  14. ↑ Douglas, MW; Li, S (1996). "Diurnal variation of the lower tropospheric flow over the Arizona low desert from SWAMP-1993 observations". Monthly Weather Review. 124 (6): 1211–1224. Bibcode:1996MWRv..124.1211D. doi:10.1175/1520-0493(1996)124<1211:DVOTLT>2.0.CO;2.
  15. ↑ "North American Monsoon Highlights". Albuquerque Weather Office, NOAA. Retrieved September 14, 2022.
  16. ↑ Rohli, Robert V.; Vega, Anthony J. (2011). Climatology. Jones & Bartlett Learning. p. 187. ISBN 978-0763791018. Archived from the original on June 19, 2013. Retrieved July 23, 2011. Although the North American monsoon region experiences pronounced precipitation seasonally, it differs from a true monsoon, which is characterized by a distinct seasonal reversal of prevailing surface winds. No such situation occurs in [North America]
  17. ↑ Cook, Ben; Seager, Richard. "The Future of the North American Monsoon".
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