References

Biogeosciences

1726-4189

Copernicus Publications

Göttingen, Germany

10.5194/bg-12-29-2015

Distribution and biophysical processes of beaded streams in Arctic permafrost landscapes

Arp

C. D.

¹ Whitman

M. S.

² Jones

B. M.

³ Grosse

https://orcid.org/0000-0001-5895-2141

⁴ Gaglioti

B. V.

¹ ³ Heim

K. C.

⁵

Water and Environmental Research Center, University of Alaska Fairbanks, Fairbanks, AK 99775, USA

Arctic Field Office, Bureau of Land Management, Fairbanks, AK 99709, USA

Alaska Science Center, U.S. Geological Survey, Anchorage, AK 99508, USA

Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Potsdam, Germany

School of Fisheries and Ocean Sciences, University of Alaska Fairbanks, Fairbanks, AK 99775, USA

06 01 2015

12 1 29 47

2015

This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit https://creativecommons.org/licenses/by/3.0/

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Beaded streams are widespread in permafrost regions and are considered a common thermokarst landform. However, little is known about their distribution, how and under what conditions they form, and how their intriguing morphology translates to ecosystem functions and habitat. Here we report on a circum-Arctic survey of beaded streams and a watershed-scale analysis in northern Alaska using remote sensing and field studies. We mapped over 400 channel networks with beaded morphology throughout the continuous permafrost zone of northern Alaska, Canada, and Russia and found the highest abundance associated with medium to high ground-ice content permafrost in moderately sloping terrain. In one Arctic coastal plain watershed, beaded streams accounted for half of the drainage density, occurring primarily as low-order channels initiating from lakes and drained lake basins. Beaded streams predictably transition to alluvial channels with increasing drainage area and decreasing channel slope, although this transition is modified by local controls on water and sediment delivery. The comparisons of one beaded channel using repeat photography between 1948 and 2013 indicate a relatively stable landform, and 14C dating of basal sediments suggest channel formation may be as early as the Pleistocene–Holocene transition. Contemporary processes, such as deep snow accumulation in riparian zones, effectively insulate channel ice and allows for perennial liquid water below most beaded stream pools. Because of this, mean annual temperatures in pool beds are greater than 2 °C, leading to the development of perennial thaw bulbs or taliks underlying these thermokarst features that range from 0.7 to 1.6 m. In the summer, some pools thermally stratify, which reduces permafrost thaw and maintains cold-water habitats. Snowmelt-generated peak flows decrease rapidly by two or more orders of magnitude to summer low flows with slow reach-scale velocity distributions ranging from 0.01 to 0.1 m s−1, yet channel runs still move water rapidly between pools. The repeating spatial pattern associated with beaded stream morphology and hydrological dynamics may provide abundant and optimal foraging habitat for fish. Beaded streams may create important ecosystem functions and habitat in many permafrost landscapes and their distribution and dynamics are only beginning to be recognized in Arctic research.

References 1

Armstrong, J. B., Schindler, D. E., Ruff, C. P., Brooks, G. T., Bentley, K. E., and Torgersen, C. E.: Diel horizontal migration in streams: Juvenile fish exploit spatial heterogeneity in thermal and trophic resources, Ecology, 94, 2066–2075, <a href="http://dx.doi.org/10.1890/12-1200.1">https://doi.org/10.1890/12-1200.1</a>, 2013.

Arp, C. D., Schmidt, J. C., Baker, M. A., and Myers, A. K.: Stream geomorphology in a mountain lake district: hydraulic geometry, sediment sources and sinks, and downstream lake effects, Earth Surf. Proc. Land., 32, 525–543, <a href="http://dx.doi.org/10.1002/Esp.1421">https://doi.org/10.1002/Esp.1421</a>, 2007.

Arp, C., Jones, B., Beck, R., Whitman, M., Derry, J., Lilly, M., and Grosse, G.: Variation in snow-water equivalent (SWE) among tundra, lakes, and streams on the Alaskan Arctic Coastal Plain: implications for regional SWE estimates and ice-thickness, Annual Conference of the American Water Resources Association, Phillidelphia, PA, November 2, 28, 2010.

Arp, C. D., Jones, B. M., Lu, Z., and Whitman, M. S.: Shifting balance of lake ice regimes on the Arctic Coastal Plain of northern Alaska, Geophys. Res. Lett., 39, 1–5, 2012a.

Arp, C. D., Whitman, M. S., Jones, B. M., Kemnitz, R., Grosse, G., and Urban, F. E.: Drainage network structure and hydrologic behavior of three lake-rich watersheds on the Arctic Coastal Plain, Alaska, Arct. Antarct. Alp. Res., 44, 385–398, 2012b.

Best, H., McNamara, J. P., and Liberty, L.: Association of ice and river channel morphology determined using ground-penetrating radar in the Kuparuk River, Alaska, Arct. Anarct. Alpi. Res., 37, 157–162, 2005.

Betts, E. and Kane, D. L.: Understanding the mechanisms by which a perennial Arctic stream appears intermittent, American Geophysical Union Fall Meeting, San Francisco, 2011.

Bowling, L. C., Kane, D. L., Gieck, R. E., Hinzman, L. D., and Lettenmaier, D. P.: The role of surface storage in a low-gradient Arctic watershed, Water Resour. Res., 39, 1087, <a href="http://dx.doi.org/10.1029/2002WR001466">https://doi.org/10.1029/2002WR001466</a>, 2003.

Brewer, M. C.: The thermal regime of an arctic lake, Transactions of the American Geophysical Union, 39, 278–284, 1958.

Brosten, T. R., Bradford, J. H., McNamara, J. P., Zarnetske, J. P., Gooseff, M. N., and Bowden, W. B.: Profiles of temporal thaw depths beneath two arctic stream types using ground-penetrating radar, Permafrost Periglac., 17, 341–355, 2006.

Brown, J.: An estimation of ground ice, coastal plain, northern Alaska, US Army Cold Regions Research and Engineering Laboratory Hanover, NH, 22, 1968.

Brown, J., Ferrians, O. J., Heginbottom, J. A., and Melnikov, E. S.: Circum-arctic map of permafrost and ground ice conditions, National Snow and Ice Data Center, Boulder, CO, 1998.

Burn, C. R.: Tundra lakes and permafrost, Richards Island, western Arctic coast, Canada, Can. J. Earth Sci., 39, 1281–1298, <a href="http://dx.doi.org/10.1139/E02-035">https://doi.org/10.1139/E02-035</a>, 2002.

Carter, L. D.: A Pleistocene sand sea on the Alaskan Arctic coastal plain, Science, 211, 381–383, 1981.

Carter, L. D. and Galloway, J. P.: Engineering Geologic Map of the Harrison Bay Quadrangle, Alaska, U.S. Geological Survey, Menlo Park, CA, 2005.

Craig, P. C. and McCart, P. J.: Classification of stream types in Beaufort Sea drainages between Prudhoe Bay, Alaska and the MacKenzie Delta, N.W.T., Canada, Arct. Alp. Res., 7, 183–198, 1975.

Crawford, R. H.: Structure of an air-breathing organ and the swim bladder in the Alaska blackfish, Dallia pectoralis Bean, Canadian Journal of Zoology, 52, 1221–1225, 1974.

Davis, N.: Permafrost: a guide to frozen ground in transition, University of Alaska Press, Fairbanks, 351 pp., 2001.

Ensom, T. P., Burn, C. R., and Kokelj, S. V.: Lake- and channel-bottom temperatures in the Mackenzie Delta, Northwest Territories, Can. J. Earth Sci., 49, 963–978, <a href="http://dx.doi.org/10.1139/E2012-001">https://doi.org/10.1139/E2012-001</a>, 2012.

Frohn, R. C., Hinkel, K. M., and Eisner, W. R.: Satellite remote sensing classification of thaw lakes and drained thaw lake basins on the North Slope of Alaska, Remote Sens. Environ., 97, 116–126, <a href="http://dx.doi.org/10.1016/j.rse.2005.04.022">https://doi.org/10.1016/j.rse.2005.04.022</a>, 2005.

Grosse, G., Jones, B., and Arp, C.: Thermokarst Lakes, Drainage, and Drained Basins, in: Treatise on Geomorphology, edited by: Schroder, J., Giardino, R., and Harbor, J., Academic Press, San Diego, 1–29, 2013.

Heim, K.: Seasonal Movements of Arctic Grayling in a Small Stream on the Arctic Coastal Plain, Alaska, M. S., School of Fisheries and Ocean Sciences, University of Alaska Fairbanks, Fairbanks, 82 pp., 2014.

Hinkel, K. M., Frohn, R. C., Nelson, F. E., Eisner, W. R., and Beck, R. A.: Morphometric and spatial analysis of thaw lakes and drained thaw lake basins in the western Arctic Coastal Plain, Alaska, Permafrost Periglac., 16, 327–341, 2005.

Jones, B. M., Arp, C. D., Hinkel, K. M., Beck, R. A., Schmutz, J. A., and Winston, B.: Arctic lake physical processes and regimes with implications for winter water availability and management in the National Petroleum Reserve Alaska, Environ. Manage., 43, 1071–1084, <a href="http://dx.doi.org/10.1007/s00267-008-9241-0">https://doi.org/10.1007/s00267-008-9241-0</a>, 2009a.

Jones, B. M., Kolden, C. A., Jandt, R., Abatzoglou, J. T., Urban, F., and Arp, C. D.: Fire Behavior, Weather, and Burn Severity of the 2007 Anaktuvuk River Tundra Fire, North Slope, Alaska, Arct. Antarct. Alp. Res., 41, 309–316, <a href="http://dx.doi.org/10.1657/1938-4246-41.3.309">https://doi.org/10.1657/1938-4246-41.3.309</a>, 2009b.

Jones, B. M., Gusmeroli, A., Arp, C. D., Strozzi, T., Grosse, G., Gaglioti, B. V., and Whitman, M. S.: Classification of freshwater ice conditions on the Alaskan Arctic Coastal Plain using ground penetrating radar and TerraSAR-X satellite data, Int. J. Remote Sens., 34, 8267–8279, <a href="http://dx.doi.org/10.1080/2150704x.2013.834392">https://doi.org/10.1080/2150704x.2013.834392</a>, 2013.

Jones, N. E.: Incorporating lakes within the river discontinuum: longitudinal changes in ecological characteristics in stream-lake networks, Can. J. Fish. Aquat. Sci., 67, 1350–1362, Doi 10.1139/F10-069, 2010.

Jorgenson, M. T. and Shur, Y.: Evolution of lakes and basins in northern Alaska and discussion of the thaw lake cycle, J. Geophys. Res., 112, 1–12, <a href="http://dx.doi.org/10.1029/2006JF000531">https://doi.org/10.1029/2006JF000531</a>, 2007.

Jorgenson, M. T., Shur, Y. L., and Pullman, E. R.: Abrupt increase in permafrost degradation in Arctic Alaska, Geophys. Res. Lett., 33, 1–4, 2006.

Jorgenson, M. T., Romonovsky, V., Yoshikawa, K., Kanevskiy, M., Shur, Y., Marchenko, S., Brown, J., and Jones, B.: Permafrost characteristics of Alaska – a new permafrost map of Alaska, Ninth International Conference on Permafrost, Fairbanks, AK, 2008.

Kanevskiy, M., Shur, Y., Jorgenson, M. T., Ping, C-L., Michaelson, G. J., Fortier, D., Stephani, E., Dillon, M., and Tumskoy, V.: Ground ice in the upper permafrost of the Beaufort Sea coast of Alaska, Cold Reg. Sci. Technol., 85, 56–70, 2013.

Lachenbruch, A. H.: Contraction theory of ice-wedge polygons: a qualitative discussion, Permaforst International Conference, Lafayette, Indiana, 63–70, 1966.

Lachenbruch, A. H., Brewer, M. C., Greene, G. W., and Marshall, B. V.: Temperatures in permafrost, in: Temperature, its Measurement and Control in Science and Industry, 791–803, 1962.

Manley, W. F. and Kaufman, D. S.: Alaska PaleoGlacier Atlas, Institute of Arctic and Alpine Research (INSTAAR), University of Colorado, Boulder, CO, 2002.

McFarland, J., Wipfli, M. W., and Whitman, M. S.: Feeding ecology of Arctic grayling in a small beaded stream on the Arctic Coastal Plain, Alaska, Conference of the Alaska Chapter of the American Fisheries Society, Kodiak, AK, 128, 23 October, 2012.

McKnight, D. M., Gooseff, M. N., Vincent, W. F., and Peterson, B. J.: High-latitude rivers and streams, in: Polar Rivers and Lakes, edited by: Vincent, W. F. and Laybourn-Parry, J., Oxford University Press, Oxford, 83–102, 2008.

McNamara, J. P., Kane, D. L., and Hinzman, L. D.: An analysis of an arctic channel network using a digital elevation model, Geomorphology, 29, 339–353, 1999.

Merck, M. F. and Neilson, B. T.: Modelling in-pool temperature variability in a beaded arctic stream, Hydrol. Process., 26, 3921–3933, <a href="http://dx.doi.org/10.1002/Hyp.8419">https://doi.org/10.1002/Hyp.8419</a>, 2012.

Merck, M. F., Neilson, B. T., Cory, R. M., and Kling, G. W.: Variability of in-stream and riparian storage in a beaded arctic stream, Hydrol. Process., 26, 2938–2950, <a href="http://dx.doi.org/10.1002/Hyp.8323">https://doi.org/10.1002/Hyp.8323</a>, 2012.

Montgomery, D. R. and Dietrich, W. E.: Source areas, drainage density, and channel initiation, Water Resour. Res., 25, 1907–1918, 1989.

Montgomery, D. R. and Buffington, J. M.: Channel-reach morphology in mountain drainage basins, Geol. Soc. Am. Bull., 109, 596–611, 1997.

Oswood, M. W., Everett, K. R., and Schell, D. M.: Some physical and chemical characteristics of an arctic beaded stream, Holarctic Ecol., 12, 290–295, 1989.

Pewé, T. L.: Ice-wedges in Alaska – classification, distribution, and climatic significance, Permafrost International Conference, Lafayette, Indiana, 1966, 76–81, 1966.

Reimer, P. J., Bard, E., Bayliss, A., Beck, J. W., Blackwell, P. G., Ramsey, C. B., Buck, C. E., Cheng, H., Edwards, R. L., Friedrich, M., Grootes, P. M., Guilderson, T. P., Haflidason, H., Hajdas, I., Hatte, C., Heaton, T. J., Hoffmann, D. L., Hogg, A. G., Hughen, K. A., Kaiser, K. F., Kromer, B., Manning, S. W., Niu, M., Reimer, R. W., Richards, D. A., Scott, E. M., Southon, J. R., Staff, R. A., Turney, C. S. M., and van der Plicht, J.: Intcal13 and Marine13 Radiocarbon Age Calibration Curves 0–50000 Years Cal Bp, Radiocarbon, 55, 1869–1887, 2013.

Rosgen, D. L.: A classification of natural rivers, Catena, 22, 169–199, 1994.

Runkel, R. L.: Using OTIS to model solute transport in streams and rivers, USGS, Denver, CO, Fact Sheet FS-138-99, 1–4, 2000.

Scott, K. M.: Effects of permafrost on stream channel behavior in Arctic Alaska, USGS, Washingtion, D. C., Geological Survey Professional Paper 1068, 1–19, 1978.

Scott, W. B. and Crossman, E. J.: Freshwater fishes of Canada, Fisheries Research Board of Canada, 966 pp., 1973.

Sturm, M., Racine, C., and Tape, K.: Increasing shrub abundance in the Arctic, Nature, 411, 546–547, 2001.

Tarbeeva, A. M. and Surkov, V. V.: Beaded channels of small rivers in permafrost zones, Geography and Natural Resources, 34, 27–32, <a href="http://dx.doi.org/10.1134/S1875372813030049">https://doi.org/10.1134/S1875372813030049</a>, 2013.

Vasudevan, D., Fimmen, R. L., and Francisco, A. B.: Tracer-grade rhodamine WT: structure of constituent isomers and their sorption behavior, Environ. Sci. Technol., 35, 4089–4096, 2001.

West, R. L., Smith, M. W., Barber, W. E., Reynolds, J. B., and Hop, H.: Autumn Migration and Overwintering of Arctic Grayling in Coastal Streams of the Arctic National Wildlife Refuge, Alaska, T. Am. Fish. Soc., 121, 709–715, <a href="http://dx.doi.org/10.1577/1548-8659(1992)121<0709:Amaooa>2.3.Co;2">https://doi.org/10.1577/1548-8659(1992)121<0709:Amaooa>2.3.Co;2</a>, 1992.

Whiting, P. J. and Bradley, J. B.: A process-based classification system for headwater streams, Earth Processes and Landforms, 18, 603–612, 1993.

Whitman, M. S., Arp, C. D., Jones, B., Morris, W., Grosse, G., Urban, F., and Kemnitz, R.: Developing a long-term aquatic monitoring network in a complex watershed of the Alaskan Arctic Coastal Plain, in: Proceedings of the Fourth Interagency Conference on Research in Watersheds: Observing, Studying, and Managing for Change, 2011–5169 ed., edited by: Medley, C. N., Patterson, G., and Parker, M. J., Scientific Investigations Report, USGS, Reston, 15–20, 2011.

Wohl, E.: Mountain Rivers, Water Resources Monograph 14, American Geophysical Union, Washington, D.C., 320 pp., 2000.

Woo, M.: Permafrost Hydrology, Springer-Verlag, New York, 563 pp., 2012.

Zarnetske, J. P., Gooseff, M. N., Brosten, T. R., Bradford, J. H., McNamara, J. P., and Bowden, W. B.: Transient storage as a function of geomorphology, discharge, and permafrost active layer conditions in Arctic tundra streams, Water Resour. Res., 43, 1–13, <a href="http://dx.doi.org/10.1029/2005WR004816">https://doi.org/10.1029/2005WR004816</a>, 2007.

Zarnetske, J. P., Gooseff, M. N., Bowden, W. B., Greenwald, M. J., Brosten, T. R., Bradford, J. H., and McNamara, J. P.: Influence of morphology and permafrost dynamics on hyporheic exchange in arctic headwater streams under warming climate conditions, Geophys. Res. Lett., 35, 1–5, <a href="http://dx.doi.org/10.1029/2007GL032049">https://doi.org/10.1029/2007GL032049</a>, 2008.