Claim · model-written summary
Southwest monsoon circulation was enhanced from 12,000 to 6000 yr BP in response to insolation peaks.
- Outcome
- southwest monsoon circulation was enhancede7
- Qualifier
- in response to peaks in annual (11,500-11,000 yr BP) and summer insolation (10,000-9000 yr BP)e7
Not reportedTaxonMaterialGeneCompoundOrgan / stageInteractorInteractor roleSecond interactorSecond interactor roleTreatmentComparatorSettingDirectionValue
Verbatim
e7“The paleoecologic record generally confirm predictions of general circulation models (GCMs) that southwest monsoon circulation was enhanced from 12,000-6000 yr BP in response to peaks in annual (11,500-11,000 yr BP) and summer insolation (10,000-9000 yr BP) during the late Quaternary.”
Title
The timing of late Quaternary monsoon precipitation maxima in the southwest United States.
David S. Shafer UA Campus Repository (The University of Arizona) 1989
Other claims from this paper (18)
- Association High percentages of Pinus and Juniperus pollen at Montezuma Well suggest a shift from winter to summer precipitation between ca. 12,000 and 9000 yr BP.
- Association Maximum influxes of Quercus and Gramineae pollen at Montezuma Well suggest a shift to summer precipitation between ca. 12,000 and 9000 yr BP.
- Observation Maximum aridity occurred between 7000 and 4000 yr BP, coincident with the lowest lake levels.
- Association High Artemisia to Chenopodiaceae-Amaranthus pollen ratios at Fryingpan Lake suggest precipitation maxima until ca. 6000 yr BP.
- Association High Artemisia to Chenopodiaceae-Amaranthus pollen ratios at Posy Lake suggest precipitation maxima until ca. 5000 yr BP.
- Observation Pinus edulis, P. ponderosa and Quercus gambelii were present on the western Colorado Plateau throughout the Holocene.
- Observation Ecotones of Pinus edulis, P. ponderosa and Q. gambelii moved upslope after ca. 6000 yr BP.
- Observation Expansion of shadscale steppe vegetation at low elevations suggests a period of maximum aridity from decreased summer precipitation.
- Observation Low lake levels between ca. 5000 and 3700 yr BP suggest a period of maximum aridity.
- Association Pollen records from Head Lake suggest an expansion of oaks and junipers at the Pleistocene/Holocene boundary that may indicate increased summer precipitation.
- Observation Lake levels of Head Lake fell sharply after ca. 9500 yr BP.
- Observation Pinus ponderosa was established in the Como Lake area by ca. 12,000 yr BP.
- Observation Pinus edulis was established in the Como Lake area by ca. 9500 yr BP.
- Observation Summer precipitation maxima may have lasted later into the Holocene on the High Plateaus, until ca. 6000-5000 yr BP.
- Observation Summer precipitation maxima may have lasted later into the Holocene in central Colorado, until ca. 4000 yr BP.
- Mechanism Regional orographic uplift may be responsible for the duration of summer precipitation maxima in the highland regions.
- Observation Sites in the southern Great Basin and Mohave Desert may have recorded enhanced summer precipitation earlier than highland sites.
- Observation The paleoecologic record generally confirms model predictions that southwest monsoon circulation was enhanced from 12,000 to 6000 yr BP.