Clovis and Toyah: Convergent Blade Technologies on the Southern Plains Periphery of North America

2019 ◽  
Vol 20 (4) ◽  
pp. 751-771 ◽  
Author(s):  
Richard Seager ◽  
Jennifer Nakamura ◽  
Mingfang Ting

AbstractMechanisms of drought onset and termination are examined across North America with a focus on the southern Plains using data from land surface models and regional and global reanalyses for 1979–2017. Continental-scale analysis of covarying patterns reveals a tight coupling between soil moisture change over time and intervening precipitation anomalies. The southern Great Plains are a geographic center of patterns of hydrologic change. Drying is induced by atmospheric wave trains that span the Pacific and North America and place northerly flow anomalies above the southern Plains. In the southern Plains winter is least likely, and fall most likely, for drought onset and spring is least likely, and fall or summer most likely, for drought termination. Southern Plains soil moisture itself, which integrates precipitation over time, has a clear relationship to tropical Pacific sea surface temperature (SST) anomalies with cold conditions favoring dry soils. Soil moisture change, however, though clearly driven by precipitation, has a weaker relation to SSTs and a strong relation to internal atmospheric variability. Little evidence is found of connection of drought onset and termination to driving by temperature anomalies. An analysis of particular drought onsets and terminations on the seasonal time scale reveals commonalities in terms of circulation and moisture transport anomalies over the southern Plains but a variety of ways in which these are connected into the large-scale atmosphere and ocean state. Some onsets are likely to be quite predictable due to forcing by cold tropical Pacific SSTs (e.g., fall 2010). Other onsets and all terminations are likely not predictable in terms of ocean conditions.


2019 ◽  
Vol 32 (17) ◽  
pp. 5417-5436 ◽  
Author(s):  
Benjamin I. Cook ◽  
Richard Seager ◽  
A. Park Williams ◽  
Michael J. Puma ◽  
Sonali McDermid ◽  
...  

AbstractIn the mid-twentieth century (1948–57), North America experienced a severe drought forced by cold tropical Pacific sea surface temperatures (SSTs). If these SSTs recurred, it would likely cause another drought, but in a world substantially warmer than the one in which the original event took place. We use a 20-member ensemble of the GISS climate model to investigate the drought impacts of a repetition of the mid-twentieth-century SST anomalies in a significantly warmer world. Using observed SSTs and mid-twentieth-century forcings (Hist-DRGHT), the ensemble reproduces the observed precipitation deficits during the cold season (October–March) across the Southwest, southern plains, and Mexico and during the warm season (April–September) in the southern plains and the Southeast. Under analogous SST forcing and enhanced warming (Fut-DRGHT, ≈3 K above preindustrial), cold season precipitation deficits are ameliorated in the Southwest and southern plains and intensified in the Southeast, whereas during the warm season precipitation deficits are enhanced across North America. This occurs primarily from greenhouse gas–forced trends in mean precipitation, rather than changes in SST teleconnections. Cold season runoff deficits in Fut-DRGHT are significantly amplified over the Southeast, but otherwise similar to Hist-DRGHT over the Southwest and southern plains. In the warm season, however, runoff and soil moisture deficits during Fut-DRGHT are significantly amplified across the southern United States, a consequence of enhanced precipitation deficits and increased evaporative losses due to warming. Our study highlights how internal variability and greenhouse gas–forced trends in hydroclimate are likely to interact over North America, including how changes in both precipitation and evaporative demand will affect future drought.


Author(s):  
Peter Mitchell

Ruled from Mexico City for about a century longer than they have thus far been from Washington, New Mexico and Arizona lie in what English speakers generally term ‘the Southwest’. I follow that usage here, even though calling them the ‘Northwest’ (of first colonial New Spain and then an independent Mexico) would, for this chapter’s purposes, be more accurate, as well as emphasizing that the cultural area to which their Indigenous inhabitants belonged extended across modern Chihuahua, Coahuila, Durango, Sinaloa, and Sonora. Together with the Southern Plains, to which trade links intimately tied it before and after Spanish arrival, the Southwest constituted the cradle within which the first Horse Nations of North America took shape. I start by highlighting key aspects of the two regions’ ecologies and prehistories. Next, I look at the horse’s impact on the Southwest’s settled farming peoples, particularly the Pueblos, many of whom came under Spanish rule after 1598. Its take-up by their Athapaskan-speaking neighbours, the Apache and Navajo, gives us our first view of how more mobile societies understood and used the horse, including—in the Navajo case—the development of a distinctive pastoralist way of life. Attention then turns to the Comanche, another pivotal player in the horse’s expansion across western North America, for whom it altered not just how they secured food, but also their social organization and entire economy. Trade—especially trade in horses—was critical in this, and so I end by examining the horse’s arrival among some of the Comanches’ trade partners, the village communities of the eastern edge of the Southern Plains, an area to which Native farmers-with-horses from the American South moved, and were forced to move, in the early 1800s. The Southwest is one of the driest parts of North America (Plate 4). Its climate is also strongly seasonal, with cold winters and hot summers. Major drainages are few: the Colorado in the west and northwest, southern Arizona’s Gila, the Río Grande, which snakes south through New Mexico and then along the present Texas/Mexico border, and the rivers draining into the Gulf of California from Mexico’s rugged Sierra Madre Occidental.


2002 ◽  
Vol 67 (1) ◽  
pp. 37-64 ◽  
Author(s):  
Susan C. Vehik

Trade is a prominent activity across much of North America during the Late Prehistoric period. On the Southern Plains, two approaches are used commonly to explain trade during this period. In one, trade is part of a system of economic interdependence between egalitarian societies having very distinct subsistence strategies. In the other, trade reflects the incorporation of Plains societies into macroeconomies centered outside the Plains. I argue that these two approaches inadequately account for Plains trade and are too narrowly constructed to account for the wider trade of which the Plains is a part. As an alternative, I propose that trade develops on the Southern Plains and elsewhere as an internally motivated political activity within the context of widespread and increasing conflict accompanied by substantial spatial rearrangements of people.


2018 ◽  
Vol 21 ◽  
pp. 1259-1265 ◽  
Author(s):  
Kristen Carlson ◽  
Leland C. Bement ◽  
Brian J. Carter ◽  
Brendan J. Culleton ◽  
Douglas J. Kennett

2010 ◽  
Vol 75 (4) ◽  
pp. 907-933 ◽  
Author(s):  
Leland C. Bement ◽  
Brian J. Carter

Clovis hunters of the North American Great Plains are known for their ability to hunt and scavenge mammoths. Less is known of their hunting strategies for other large animals, such as horse, camel, and bison, although remains of these animals have been found at several Clovis camps. Recent investigations of the Jake Bluff site on the southern Plains have identified a Clovis bison kill in an arroyo. The apparent use of an arroyo style trap for bison hunting provides the opportunity to study Clovis hunting strategies that came to be widely used during later Paleoindian times. The arroyo style bison trap is generally attributed to Folsom and later groups, and yet the Jake Bluff site yielded an association of Clovis-style projectile points with the remains of 22 Bison antiquus at the bottom of a short arroyo. The late date of 12,838 cal. BP suggests that the site spans the gap between the Clovis mammoth hunter and the Folsom bison hunter, indicating that some Clovis hunters developed the arroyo style bison trap to capture multiple bison at the same time, and as mammoths were extirpated from certain areas during the Pleistocene to Holocene transition.


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