Lake Waiau

{{short description|Lake in Hawaii, United States}}

{{Infobox body of water

| name = Lake Waiau

| image = Lake Waiau2.jpg

| alt = Lake Waiau

| caption =

| image_bathymetry =

| caption_bathymetry =

| location = Mauna Kea, Hawaii

| coords = {{coord|19.81125|-155.47743|format=dms|type:waterbody_region:US-HI|display=inline,title}}

| type =

| inflow =

| outflow =

| catchment = {{convert|13.5|ha|abbr=on}}

| basin_countries = United States

| length =

| width = {{convert|100|m|abbr=on}}

| area = {{convert|6000|m2|abbr=on}}

| depth =

| max-depth = {{convert|2|-|2.5|m|ft|abbr=on}}

| volume =

| residence_time =

| shore =

| elevation = {{convert|3970|m|abbr=on}}

| islands =

| cities =

| pushpin_map = Hawaii#Pacific Ocean

| pushpin_label_position =

| pushpin_map_alt = Location of Lake Waiau in Hawaii, US

| pushpin_map_caption =

| website =

| reference =

}}

Lake Waiau{{GNIS|364585|Lake Waiau}} is a high-elevation lake located at {{convert|3970|m|ft|abbr=on}} above sea level on Mauna Kea, on the island of Hawaiʻi. It is arguably one of the highest lakes in the United States.{{cite web|url=http://www.highestlake.com/highest-lake-usa.html#Waiau |title=The Highest Lake in the USA |accessdate=2008-10-11}} After the evaporation of Ka Wai o Pele in 2018 and the short-lived lake in Halemaʻumaʻu crater in 2020, Lake Waiau is the only lake on Hawaiʻi Island and one of very few lakes at all in the state of Hawaiʻi. It is relatively small, only about 100 m across, and varies in size as the water level rises and falls. At high water levels a small outlet stream appears at the northwest end, but it is absorbed into the ground after a short distance. The name means "swirling water" in Hawaiian, though it is usually rather placid. It usually freezes in winter, but aquatic insects such as midges and beetles can be found breeding in the water.

Description

Lake Waiau is located inside the Pu'u Waiau cinder cone at an altitude of 3970 m. It is approximately heart shaped and its diameter reaches about 100 m. The average surface area of the lake is around {{cvt|6000|m2|ft2 ha acre}}. The size of its surface area fluctuates significantly over the year. It reaches its peak during spring with a maximal depth between 2 m and 2.5 m. By the end of the summer, it often has shrunk to one third of its original size with a maximal depth below 1 m. A spillover into the Pohakuloa Gulch occurs when the lake depth is more than 2.3 m. The lake is only fed by precipitation, which occurs primarily during the winter; its catchment area is about {{cvt|135000|m2|ft2 ha acre}}, mostly located within the Pu'u Waiau cinder cone.

The lake is an anomaly in the peak region of Mauna Kea as everywhere else the ground is unable to retain water. The exact nature of the impermeable ground layer of the lake is still unknown. It is assumed that fine-grained densely compressed ash, basalt rock or a small permafrost layer may play a role. No permafrost layer has been established so far for the lake area itself, but it was found at another location in the peak area. The bottom of the lake, however, is known to have a {{convert|7.5|m|adj=on}} thick sediment layer.

Temporary shrinkage 2010-2014

Between 2010 and 2013 the lake shrank significantly. On 26 September 2013, the lake had been reduced to a mere puddle of less than 2% of its original surface size, with a reported width of {{cvt|10|yd|m|order=flip|0}} and maximum depth of {{cvt|9|in|cm|order=flip|0}}. By December 2013, three months later, the maximum depth had dropped further to {{cvt|5|in|cm|order=flip|0}}.Jensen, Chelsea (2020-07-25). Lake Waiau remains full. West Hawaii Today, 25 July 2020. Retrieved from https://www.westhawaiitoday.com/2020/07/25/hawaii-news/lake-waiau-remains-full-2/.

The exact causes for the water loss are unknown. The suspects are drought conditions and the thawing of an assumed permafrost layer under the lake leading to increased seepage.

After the particularly wet winter of 2013/2014, however, the lake was back to around 75% of its original size by May 2014, and subsequently returned to its normal size. The drought conditions on Mauna Kea from 2010 to 2013 are currently believed to have been the primary reason for the water loss.{{cite web|author=Jensen, Chelsea|url=http://westhawaiitoday.com/news/local-news/lake-waiau-atop-mauna-kea-nearly-full-or-full-fall-2014 |title=Lake Waiau atop Mauna Kea nearly full or full since fall 2014 |date=2017-03-22 |archiveurl=https://web.archive.org/web/20170329232828/http://westhawaiitoday.com/news/local-news/lake-waiau-atop-mauna-kea-nearly-full-or-full-fall-2014 |archivedate=2017-03-29 |website = West Hawaii Today }}

Mythology

The lake is of some importance in Hawaiian mythology. Aside from Poliʻahu, there are two additional snow deities, Lilinoe and Waiau, who are associated with Mauna Kea, and according to Westervelt, the lake was probably named after the goddess of the same, who used to bathe in it. Originally Hawaiians considered the whole peak region of Mauna Kea, including Lake Waiau, a sacred site, and only priests and chieftains were allowed to access it. Later, after the formation of the Hawaiian kingdom, the peak region was occasionally visited by members of the royal family. The last one to do so was Queen Emma in 1881, who also took a bath in the lake during her visit.

Gallery

File:Lake Waiau3.jpg|view from above

File:Lake Waiau person.jpg|with a person for scale

File:Lake Waiau outlet2.jpg|outlet stream

File:Lake Waiau at Mauna Kea - panoramio.jpg|Shrinkage October 2012

File:Lake Waiau Panorama.jpg|May 26, 2019

See also

References

Ehlmann, Bethany L.; Raymond Arvidson,; Bradley Jolliff,; Sarah Johnson,; Brian Ebel,; Nicole Lovenduski,; Julie Morris,; Jeffery Byers,; Nathan Snider,; Robert Criss,. Hydrologic and isotopic modeling of alpine Lake Waiau, Mauna Kea, Hawai'i. (1). Pacific Science. 2005. {{Webarchive|url=https://web.archive.org/web/20140611070700/http://www.highbeam.com/doc/1G1-129714347.html |date=2014-06-11 }}

Disappearing Lake Waiau Is a Mystery to Scientists. Honolulu Star – Advertiser. 2013. (February 16, 2014). [https://www.questia.com/read/1P3-3122526991]{{dl|date=July 2021}}

Alan C. Ziegler: Hawaiian Natural History, Ecology, and Evolution. University of Hawaii Press, 2002, {{ISBN|0824821904}}, S. 94 ({{Google books|l56J_8teG58C|excerpt|page=94}})

H. Arlo Nimmo: Pele, Volcano Goddess of Hawai'i: A History. McFarland, 2011, {{ISBN|9780786463473}}, S. 28 ({{Google books|n2ii6J0C0hYC|excerpt|page=28}})

[http://www.ifa.hawaii.edu/info/vis/culture.html Hawaiian Culture & Mauna Kea] {{webarchive|url=https://archive.today/20140222014840/http://www.ifa.hawaii.edu/info/vis/culture.html |date=2014-02-22 }} auf den Webseiten der Mauna Kea Visitor Information Station; retrieved, 22 February 2014)

Erin Miller: [http://hawaiitribune-herald.com/news/local-news/rise-lake-waiau-benefits-wetter-weather On the rise: Lake Waiau benefits from wetter weather] {{Webarchive|url=https://web.archive.org/web/20140820001137/http://hawaiitribune-herald.com/news/local-news/rise-lake-waiau-benefits-wetter-weather |date=2014-08-20 }}. Hawaii Tribune Herald, 30. Mai 2014

Bibliography

  • Jane Ellen Massey: Lake Waiau: A Study of a Tropical Alpine Lake, Past and Present. University of Hawaii Press, 1978
  • Alfred H. Woodcock, Meyer Rubin, R. A. Duce: Deep Layer of Sediments in Alpine Lake in the Tropical Mid-Pacific. Science, New Series, Vol. 154, No. 3749 (Nov. 4, 1966), pp. 647–648 ([https://www.jstor.org/stable/1719061 JSTOR])