the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
03 Sep 2021
03 Sep 2021
Holocene climate and oceanography of the coastal Western United States and California Current System
- 1Earth and Planetary Sciences Department, University of California, Davis, Davis, California, 95616, United States of America
- 2Bodega Marine Laboratory, University of California, Davis, Bodega Bay, California, 94923, United States of America
- 1Earth and Planetary Sciences Department, University of California, Davis, Davis, California, 95616, United States of America
- 2Bodega Marine Laboratory, University of California, Davis, Bodega Bay, California, 94923, United States of America
Abstract. To understand and contextualize modern climate change, we must improve our understanding of climatic and oceanographic changes in the Holocene (11.75 ka–present). Climate records of the Holocene can be utilized as a “baseline” from which to compare modern climate and can also provide insights into how environments and ecosystems experience and recover from environmental change. However, individual studies on Holocene climate in the literature tend to focus on a distinct geographic location, a specific proxy record, or a certain aspect of climate (e.g., upwelling or precipitation), resulting in localized, record-specific trends rather than a comprehensive view of climate variability through the Holocene. Here we synthesize the major oceanographic and terrestrial changes that have occurred in the Western United States (bounded by 30° N to 52° N and 115° W to 130° W) through the most recent 11.75 ka and explore the impacts of these changes on marine and terrestrial ecosystems and human populations. This three-tiered systematic review combines interpretations from over 100 published studies, codes and geospatially analyzes temperature, hydroclimate, and fire history from over 50 published studies, and interprets nine representative time series through the Holocene. We find that the early Holocene is characterized by warming relative to pre-Holocene conditions, including warm sea surface conditions, a warm and dry Pacific Northwest, a warm and wet Southwest, and overall spatial and temporal stability. In the mid Holocene, these patterns reverse; this interval is characterized by cool sea surface temperatures, a cool and wet Pacific Northwest and warm and dry Southwest. The late Holocene is the most variable interval, both spatially and temporally, and a novel spatial trend appears in terrestrial climate with warmer coastal areas and cooler inland areas. Human communities interacted with the environment throughout the entire Holocene, as evidenced in archeological and paleoenvironmental records, yet the recent era of colonization (1850–present) represents an unprecedented environmental interval in many records. Overall, our analysis shows linkages between terrestrial and oceanographic conditions, distinct environmental phases through time, and emphasizes the importance of local factors in controlling climate through the dynamic Holocene.
Hannah M. Palmer et al.
Status: open (extended)
-
CC1: 'Comment on cp-2021-109', John Barron, 11 Sep 2021
reply
The article does good job of summarizing research on the Holocene evolution of the California Current and its affect on the climate of California. Graphics suggesting the driving forces behind this change, such as a plot of insolation change during the Holocene, would be beneficial.
As a researcher cited, I’d like to make some observations. Our studies (Barron et al., 2003, 2019; Addison et al., 2018) suggest the cool-water, upwelling regime of the California Current narrowed during the late Holocene (~3 ka) off northern and central California, possibly in response to intensification of the North Pacific Gyre Oscillation (NPGO). Testing of this hypothesis requires multiple core transects across the California Current, particularly south of Monterey where detailed Holocene records are lacking, as well as independent means of documenting the Holocene evolution of the NPGO.
Studies to the south needed, particularly in the region south of Monterey and north of Point Conception. The Santa Barbara Basin is shoreward of California Current and appears to feel the intensification of springtime upwelling at about 4 ka. Further south, off Baja California, warming of surface waters at ~4 ka has been tied to intensification of ENSO in MV99-GC41/PC14 by Marchitto et al. 2010; Science , 330). Increased opal MAR in that core also occurs at ~4 ka (Arellano-Torres et al., 2019, doi:10.1029/2018PA003479), seems to confirm that warmer SSTs, a likely indictor of enhanced ENSO expression, and increased upwelling are closely linked within the California Current.
At the same time, this ~4 ka step in the intensification of the California Current likely signals a major decline in the influence of the North American Monsoon (NAM) in southern California. The initiation of NAM decline at ~ 8 ka is proposed by Barron et al., 2012 (doi:10.1029/2011PA002235).
It is also important to note that seasonal bias of various proxies as well as the physical setting of a given core within the California Current can make comparison of Holocene records complicated. The seasonal biases of various surface water proxies tend to become more apparent during the late Holocene, as modern seasonal variation coupled with a narrowing California Current becomes more pronounced. For example, diatoms typically increase their flux to the sediments during the spring-summer upwelling season; however, Fragilariopsis doliolus, a subtropical diatom associated with the North Pacific Gyre, increases in relative abundance during September and October, during a period of reduced upwelling. Expression of this late Holocene change in diatom an assemblage off northern California is proposed by (Barron et al., 2003), but this hypothesis needs further testing.
Alkenones are thought to record average seasonal SSTs near the California coast vs. winter SSTs in gyre settings (Herbert in Barron et al., 2003). Therefore, comparison of diatom and alkenone SST proxies in different settings likely will differ. Similarly, as planktic foraminiferal habitats extend deeper in the water column, various SST proxies (assemblages, oxygen isotopes, Mg/Ca ratios) are likely to vary in different settings and over the course of a given Holocene record.
-
RC1: 'Comment on cp-2021-109', Anonymous Referee #1, 03 Nov 2021
reply
The paper by Palmer et al. compiles 101 papers (although the abstract says 100 plus 50?) from the western US to summarize millennial-scale (EH, MH, and LH), spatial patterns of climatic, ecologic, pyrogenic, and oceanic changes. Overall, I found the paper interesting and applaud its titanic effort. Summarizing data is not easy. The authors do a good job covering the literature with very few exceptions (see below and attached PDF). The methods are sound, the criteria for inclusion reasonable, and the final spatial and temporal interpretations within the bounds of the available science. Note: as a summary paper, I trust that the interpretations by the authors follow those by the primary authors, so I did not double the cited literature.
I provide suggestions/edits/comments below in order of the text, not importance.
1) line 48: under-sampled because of a lack of temperature-sensitive terrestrial records...I think this qualifier should be mentioned. Most WNA records are more water sensitive.
2) line 57: summer insolation was at a Holocene maximum...winter insolation was at a Holocene minimum.
3) add Kaufmann et al., 2020, and Routson et al., 2019.
4) up-date with Swain et al., 2018; Goss et al., 2020 - specific to W US and CA.
5) line 85: need to mention Wise's dipole work since it is the dominant feature of interannual hydroclimate in the W US...also, Dettinger and Cayan...also worth adding something about atmospheric rivers in this section since they are THE source of major hydrologic change - feast or famine W US climate.
6) line 125 - not sure if this Kirby paper actually deals with plant or animal communities? Maybe Kirby et al. (2018) show a strong coupling between hydroclimate and vegetation over 32,000 years at Lake Elsinore? Or, Dingemans et al. (2014)?
7) line 141: because of diverse age control issues between and within the 100 comparison sites, you might qualify this first question to reflect millennial-scale patterns since less than millennial is unlikely without significant age control assumptions across sites?
8) Figure 1: I would prefer a labeling scheme for each site so that the reader can go back and forth from the table to the figure to find the sites...e.g., 1, 2, 3, etc.
9) Figure 1: draw the boundaries as defined by your spatial criteria...PNW, SW, etc...
10) line 163: I think there should be an age control criterion...what is the minimum number of Holocene ages required to make millennial-scale statements??
11) line 163: are you updating the age models? In many of these types of summary papers, the age models are outdated and likely obsolete. Most review papers begin with fresh age models to make sure that papers published 20 years ago are correctly compared to papers published yesterday.
12) line 210: Add Leidelmeijer et al. (2021) - Barley Lake early Holocene.
13) line 230-234: in the SW (west of AZ), a wetter early Holocene was a product of more intense winter ppt associated with low winter insolation...the monsoon plays little if any significant role in the annual hydrologic budget west of AZ...see Kirby et al. (2005, 2007, 2012) and (Bird et al., 2010). It is reasonable that the monsoon boost may have "helped" maintain lakes where playas exist today, but without the increase in early Holocene winter ppt caused by lower winter insolation and its likely impact of storm tracks, the SW (west of AZ) would have been dry.
14) Figure 2: add numbers so that the reader can cross-reference sites to the table.
15) line 240: Leidelmeijer et al., 2021 agrees with a dry early Holocene from Nor Cal.
16) line 266: see earlier comments...the monsoon provided a hydrologic buffer, but it cannot explain the general increase in moisture...winter ppt must be the answer because the climate of the SW (west of AZ) is unimodal and dominated by winter ppt. All the monsoonal rain in the “world [hyperbole]” could not make the SW (west of AZ) wet without ample winter ppt...enhanced by lower winter insolation and its likely modulation of winter season storm tracks over the SW during the early Holocene.
17) line 306: add Barber, Donald C., A. Dyke, Claude Hillaire-Marcel, Anne E. Jennings, John T. Andrews, Maclean W. Kerwin, Guy Bilodeau et al. "Forcing of the cold event of 8,200 years ago by catastrophic drainage of Laurentide lakes." Nature 400, no. 6742 (1999): 344-348.
18) line 415 and elsewhere: I think you are overplaying the significance of the monsoon on the CA annual hydrologic budget. CA is characterized by a unimodal hydroclimate in terms of what matters for its annual hydrologic budget...and what matters is simply winter ppt amount and to a lesser extent, summer evaporation.
19) line 417: most of CA receives no significant monsoonal ppt ever...except Mojave and east (see Hereford, Richard, Robert H. Webb, and Claire I. Longpre. Precipitation history of the Mojave Desert region, 1893-2001. No. 117-03. 2004.).
20) Section 3.2.5 and other human sections: check out...Grenda, Donn R., and Alex V. Benitez. Continuity and change: 8,500 years of lacustrine adaptation on the shores of Lake Elsinore. Statistical Research, 1997.
21) line 628: the Late Holocene Dry Period is reserved for the published LHDP by Mensing et al. 2013...I think you misinterpreted Lund and Platzman's data and LHDP age range...at Zaca Lake, ALL 3 papers show an LHDP period between 2500 and 2000 cal yr BP. The MCA is also present as well as the LIA...but nothing comes close in duration or magnitude as the LHDP.
22) section 3.5: add Crawford, Jeffrey N., Scott A. Mensing, Frank K. Lake, and Susan RH Zimmerman. "Late Holocene fire and vegetation reconstruction from the western Klamath Mountains, California, USA: A multi-disciplinary approach for examining potential human land-use impacts." The Holocene 25, no. 8 (2015): 1341-1357.
23) line 838: really should consistently point out that the early Holocene was characterized by both higher summer insolation and lower winter insolation...BOTH played a role in the millennial-scale Holocene changes you discuss in this paper.
24) line 862: AND, age control issues!!!, proxy sensitivity issues, and differences in the proxies used from site to site.
Hannah M. Palmer et al.
Hannah M. Palmer et al.
Viewed
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 521 | 111 | 9 | 641 | 4 | 5 |
- HTML: 521
- PDF: 111
- XML: 9
- Total: 641
- BibTeX: 4
- EndNote: 5
Viewed (geographical distribution)
| Country | # | Views | % |
|---|
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1