Hawaiian Knowledge of Water

I learned this oli (chanting) this week, and I felt amazing that how ancient Hawaiian saw a big picture of the water/hydrological cycle, and then turned it into education, into art.  For Hawaiian, water is wealth (waiwai), water made the law (kānāwai).  I was impressed that the hydrology in Hawaiʻi is expressed by only one oli. It mentions about the moisture from the ocean, the evapotranspiration from the solar, the orographic rainfall in the windward side with steep mountain, the heavy rainfall or storm events sometimes, and the groundwater storage. I wonder how many people nowadays have this picture in mind that everything is linking together, and if we mess up one part of the cycle, weʻre going to mess up the entire cycle. We need a better water management for the shrinking water resources with increasing population, yet how we can maxima the benefit to society, environment, and offspring is one of the important things to figure out…

 

This is the oli – Aia i hea ka wai a Kāne (http://www.kumukahi.org/units/ke_ao_akua/akua/kane)

He ui, he nīnau, e ui aku ana au iā ʻoe: Aia i hea ka wai a Kāne?
Aia i ka hikina a ka lā puka i Haʻehaʻe;
Aia i laila ka wai a Kāne.

E ui aku ana au iā ʻoe: Aia i hea ka wai a Kāne?
Aia i kaulana a ka lā,
I ka pae ʻōpua i ke kai,
Ea mai ana ma Nihoa,
Ma ka mole mai o Lehua;
Aia i laila ka wai a Kāne.

E ui aku ana au iā ʻoe: Aia i hea ka wai a Kāne?
Aia i ke kuahiwi,
I ke kualono,
I ke awāwa,
I ke kahawai;
Aia i laila ka wai a Kāne.

E ui aku ana au iā ʻoe: Aia i hea ka wai a Kāne?
Aia i kai, i ka moana,
I ke kualau, i ke ānuenue,
I ka pūnohu, i ka ua koko, i ke ao lewalewa;
Aia i laila ka wai a Kāne.

E ui aku ana au iā ʻoe: Aia i hea ka wai a Kāne?
Aia i luna ka wai a Kāne,
I ke ao uli, i ke ao ʻeleʻele,
I ke ao panopano, i ke ao pōpolohua mea a Kāne lā ē;
Aia i laila ka wai a Kāne.

E ui aku ana au iā ʻoe: Aia i hea ka wai a Kāne?
Aia i lalo, i ka honua, i ka wai hū,
I ka wai kau a Kāne me Kanaloa,
He wai puna, he wai e inu, he wai e mana, he wai e ola.
E ola nō ā!

 

Translation:

A question, a query, I am asking you: Where are the waters of Kāne?
At the rising of the sun at Haʻehaʻe;
There are the waters of Kāne.

I am asking you: Where are the waters of Kāne?
In the resting place of the sun,
In the cloud bank over the ocean,
Rising up above Nihoa,
From the taproot of Lehua;
There are the waters of Kāne.

I am asking you: Where are the waters of Kāne?
On the mountains,
On the ridges,
In the valleys,
In the rivers;
There are the waters of Kāne.

I am asking you: Where are the waters of Kāne?
In the seas, in the ocean,
In showers from the ocean, in the rainbow,
In the low–lying rainbow, in the red rainbow, in the floating clouds;
There are the waters of Kāne.

I am asking you: Where are the waters of Kāne?
The waters of Kāne are above,
In the dark clouds, in the black clouds,
In the thick clouds, in the dark purple clouds of Kāne.
There are the waters of Kāne.

I am asking you: Where are the waters of Kāne?
Down below, in the earth, are the rising waters,
The water placed by Kāne and Kanaloa,
Spring water, drinking water, the water of divine powers, life-giving water.
Let there be life!

 

 

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Mystery of the 3 USGS Gages in Mānoa

The runoff ratio is how much runoff responses to the rainfall. Here, we use the NCDC HMNL rainfall data (the diamond symbol in Waihi subwatershed on the Annual Rainfall Map), and 3 USGS gages and their information of the drainage areas.

Why do we need drainage area? Because both of runoff and rainfall represents as depth over the watershed area. (Notice the tricky part here: we assume both of runoff and rainfall depths are well-distributed/homogeneous, but they are usually not…)

Waihi Runoff Ratio

Waihi runoff ratio shows an extreme runoff response to the rainfall, which may indicate:

  • Waihi watershed has a very permeable surface with a threshold for overland flow (Wikipedia: overland flow).
  • Either runoff or rainfall is not well-spatially (homogeneously) distributed

Besides, we can also notice that the runoff ratio excessed 100% sometimes, which means the runoff we got is more than the rainfall we observed. It whispers to us: either rainfall or runoff is not well-spatially distributed  OR there is some extra water pouring into the stream.

Waihi_runoff_ratio.png

Waiakeakua Runoff Ratio

With a similar drainage area, Waiakeakua’s runoff response more to the rainfall than Waihi’s runoff! Moreover, there were more runoff ratios larger than 100%… It looks not like only because of inhomogeneous of runoff or rainfall, but more likely some additional water input to the Waiakeakua stream.

Waiakeakua_runoff_ratio.png

Mānoa-Woodlawn Runoff Ratio

Surprisingly, Mānoa-Woodlawn runoff ratio has a similar pattern with Waihi but not Waiakeakua. I’d like to guess that there were more groundwater discharge to the Waiakeakua streams, but not Waihi and Mānoa streams. I wonder, which stream has more groundwater discharge since USGS Waiakeakua gage is actually the confluence of three streams.

Manoa_Woodlawn_runoff_ratio.png

 

Hydrograph of 3 USGS Gages in Mānoa

A hydrograph is a time-series graph showing the rate of streamflow (discharge) a specific point in a river, a stream, or another channel. We can understand the streamflow rate changes with time at the point in the stream by a hydrograph.

The streamflow is related to rainfall, thus we like to put them together and see. However, we notice that the stream gage and rain gage usually are not at the same point. For example, in Mānoa watershed, we have three stream gages but only one rain gage (see the Mānoa Annual Rainfall Map in Map Page). It is such a pain for hydrologist…(now we should learn that nature is not a separated system, we better communicate with different field first, and then set up our observation stations…) Moreover, a stream gage is at a point of a stream, but it collects all the runoff (the water flow) from the entire watershed. Besides, point rainfall cannot represent the rainfall in entire watershed, neither. Thus we have to be very aware while we’re interpreting the rainfall and streamflow at each stream gage.

Waihī USGS Stream Gage

Waihī stream gage is the one closest to the rain gage, so the streamflow responses to the rainfall should be the most accurate within three stream gages. The minimum discharge (flow) at Waihi gage is about 0.002 cms on 2/11/2012, which is almost no flow…, and the maximum discharge is 6.8 cms on 12/13/2011 during the data period. The mean discharge of Waihi gage is about 0.09, which is more than three times ‘Aihualama stream. It’s very obvious that the streamflow didn’t response to the rainfall the same way (sometimes larger discharge with larger rainfall, but sometimes more rainfall has okay discharge)

Waihi_rainfall_hydrograph.png

Waiakeakua USGS Stream Gage

Waiakeakua stream gage has mean discharge 0.13 cms, including minimum discharge, 0.037, on 1/17/2014 to 1/20/2017 and maximum discharge, 1.71 cms on 9/15/2015. We noticed that the discharge from Waiakeakua is not as extreme as Waihī. There are some possibilities:

  1. There is more groundwater discharge into Waiakeakua stream (since the minimum discharge at Waiakeakua is much higher than the minimum discharge at Waihī)
  2. The rainfall amount is not the same at Waihī and Waiakeakua, especially heavy rainfall (because the maximum discharge at Waiakeakua is much lower than the maximum discharge at Waihī)
  3. The flow paths are different in each watershed. The flow paths influence the time the water stays on or in the ground until it goes into the stream.
    • The slopes of each watershed are different. I think that the discharge will increase immediately if the slope is steeply toward to the stream.
    • Geology and soil distributions lead the distribution of infiltration rate. The infiltration rate plays an important role in the flow paths.
    • The shapes of each watershed are different. The water paths may also related to the shape of a watershed.

Waiakeakua_rainfall_hydrograph.png

Mānoa-Woodlawn USGS Stream Gage

Mānoa-Woodlawn stream gage has much higher discharge than Waihī and Waiakeakua because of its larger drainage area that allows the stream gain more water. The maximum discharge, 8.27 cms, occurred on 7/24/2016, and minimum discharge, 0.057, occurred on 12/8/2012.

Manoa_Woodlawn_rainfall_hydrograph.png

 

(All the figures in this post are from Yu-Fen through R programming, the rainfall data is from NCDC, and discharge data is from USGS)

‘Aihualama Stream

 

‘Aihualama Stream is a very small stream (we even can’t see the stream from google map). In normal days, the stream width is less than 3 m (9.84 ft) with mean discharge 0.021/0.74 cubic meter per second/cubic feet per second (cms/cfs). With mean daily rainfall, 10.7 mm (0.42 inches), the mean discharge of the Mississippi rever is 16791.8 cms (593000 cfs). [Note: the rainfall data is from NOAA’s National Climatic Data Center (NCDC); the data of ‘Aihualama Stream is from Tsang Hydrology Lab]

Although ‘Aihualama is small, don’t ignore the power of our mother nature! The streamflow can increase rapidly during a rainfall event (the discharge can hit 20 times of normal discharge during hours!!! So be careful while you’re hiking on a rainy day in Hawaii!!!). The first figure below is showing the stream on a normal day, and water can reach the orange lines during a rainfall event. As Oki (2003) pointed out, Hawaiian streams are very flashy, ‘Aihualama is not excluded (see the second picture below)

InkedIMG_8950_LI.jpgIMG_7882.JPG

Stream Ecosystem

So, who lives in this extreme flow amount stream? I guess the stream animals must have the ability to hide or hold tightly on the bottom that they won’t be flush away from a high, fast and turbulent flow. Besides, they have to tolerate the small amount of stream flow, which may cause the larger fluctuate in temperature, discontinuous stream and smaller habitat.

I saw a lot of small suckermouth armored catfishes in pools (not showing here), and crayfishes (the first photo below), guppies along the entire stream. They’re considered as invasive species for Hawai’i; they occupied the stream, and some of them eat the native species’ eggs (Devick 1989) . Also, there is an argument saying invasive fishes would impact the nutrient content and water quality in streams (Nico 2006; Capps et al. 2009)

Did I only see invasive fishes in ‘Aihualama stream? Well, I still see one or two o’opu (as the second photo), Hawaiian native goby, in the pool within like more than 30 catfishes…

On the stream bank, I saw a green and black poison dart frog (Dendrobates auratus) (the third photo below), this small tree frog is native to Central and South America. As their name implies, blow darts were rubbed on the back of frogs by indigenous tribes to make poison-tipped darts. They were introduced to Manoa Valley in the 1950s to control mosquitoes; however I didn’t find any evaluation for its consequence. More and more…. I ALWAYS GOT MOSQUITO BITTEN every time I went there…

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Black small mushrooms (?) on a dead wood across the ‘Aihualama stream… I don’t know the name of the mushrooms, but it smelled not good…

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Human Activities

On the right bank of ‘Aihualama stream at Lyon Arboretum, there are lo’i (taro farm; the first picture below), which is a part of Hawaiian cultural practicing. Some people and students go there every Wednesday to plant kalo (taro). For the farming, they need to divert the stream water into their farms, thus they use pipes (the second and third photo below) to divert the stream water into their lo’i. Most of the streams in Hawaiian are diverted for agriculture purpose; however, the water issues and conflicts increased during and after the sugar cane and pineapple plantations. How we manage the water resources and communicate with our friends living together are big challenges for us…

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Reference

Capps, K.A. and Flecker, A.S., 2013, October. Invasive aquarium fish transform ecosystem nutrient dynamics. In Proc. R. Soc. B (Vol. 280, No. 1769, p. 20131520). The Royal Society.

Devick, W.S., 1989. Disturbances and fluctuations in the Wahiawa Reservoir ecosystem. Honolulu: Hawaii Department of Land and Natural Resources, Division of Aquatic Resources.

Nico, L., Fuller, P., Cannister, M. and Neilson, M., 2006. Pterygoplichthys disjunctivus. USGS Nonindigenous Aquatic Species Database, Gainesville, FL. Revision Date, 4(21), p.2006.

Oki, D.S., 2003. Surface water in Hawaii. US Department of the Interior, US Geological Survey.

(All the photo in this post were taken by Yu-Fen Huang/yfhuang)

The “shaka sloth” I met along the stream! 😀IMG_8972.JPG

USGS Gages in Mānoa

If we want to have a better understanding for a stream, or even have the abilities to manage a stream and water resources, we need a quantitative analysis. The data from stream gages will definitely help us to figure out how much flow/stream water we have.

U.S. Geophysical Survey (USGS) has 7 gages in Mānoa-Pālolo watershed (as the map below, including 4 in Mānoa, 2 in Pālolo, and one at the confluence of both). Since we’re going to focus on the Mānoa watershed first, three USGS gages have been selected:

  1. Waihi Stream gage: the confluence of ‘Aihualama, Lua’alaea and Waihi streams
  2. Waiakeakua Stream gage: the confluence of Wa’aloa, Naniuapo and Waiakeakua streams
  3. Manoa Stream at Woodlawn Drive gage: the confluence of Waihī and Waiakeakua streams
  4. (We don’t include the Manoa Stream at Kanewai Field gage because of it only have data for few days)

usgs_gages.jpg

Gage Data Ability

The data ability of streamflow (discharge) data and water quality of 3 gages are listed below (current: 15-min interval discharge; daily: daily discharge; water quality data only provides few days in years):

usgs_gage_ability.PNG

 

Streamflow Summary

The stream summary from the USGS, and I converted the unit here. According to the drainage areas of each stream are very small comparing to the drainage areas in the Continental U.S. (CONUS). Besides, the maxima and minima of the streams also show the extreme streamflow condition, which may impact on the niches or habitat of the stream shrimps, fishes, and other. Baseflow indicates the permanent flow contributing to the total streamflow, and quick flow indicates the stormflow contributing to the total streamflow. The Waiakeakua stream has higher baseflow contribution than quick flow contribution may because it has groundwater discharge into the stream.

streamflow_summary.PNG

 

 

Mānoa Watershed – Where Mo’o live

Mānoa watershed starts with 6 streams and down to Waikiki (Ala Wai Canal after 1920):
(from Eva side toward Diamond Head side)
1. ‘Aihualama
2. Lua’alaea
3. Waihī
4. Wa’aloa
5. Naniu’apo
6. Waiakeakua

In the past, the entire Mānoa valley was full of lo’i (taro farm) because the valley is wide and flat, which is suitable for irrigation. (Sterling and Summers 1978)

Mo’o (water lizard) is one of aumakua (ancestral gods). Mo’o loves to live in rainy cliffs, mountain peaks, waterfalls, springs, streams, and pools of Mānoa (Sterling and Summers 1978). Mo’o likes wet environment; the upper Mānoa receives plenty rainfall as the previous folk story, Princess of Mānoa told us. Also, if we can check Hawaiian Rainfall Atlas, we will realize that the annual rainfall on the top of Mānoa is about 3900 mm (153.5 inches).

Mānoa was known for mo’o water spirits. They were usually shown in females with the form of large lizards. Mo’o controls water resources of  Mānoa valley, and usually brought the blessing of fish harvest, health to people, and welfare to the family and their friends. (Kamakau et al.1964).

Manoa_Head_Stream.PNG

Kōnāhuanui — Home of Mo’o

Reference

Sterling, E.P. and Summers, C.C., 1978. Sites of Oahu. Bishop Museum Pr.

Kamakau, S.M., Barrère, D.B. and Pukui, M.K., 1964. Ka Poʻe Kahiko: The People of Old. Bishop Museum Press.

Waihi Stream – Mānoa Fall

Instead of visiting Waiakeakua first, I visited Mānoa fall, Waihi Stream. According to my friend, Waiakeakua is more challenging, and my adventure friend got sick on the date that we were planning to visit Waiakeakua stream.

Mānoa fall belongs to Waihi Stream, and it’s an easy trail but very muddy…

Tropical and rainforest plants:R0015235.JPG

Mānoa fall! We heard that it’s better not to swim in the pool because of the bacteria… 😦R0015247.JPG

 

We found a way to climb up and tried to get to the top of Mānoa fall. :p1452110_567732963305683_381069119_n.jpg

The top of Mānoa fall! 😀R0015256.JPG

Only a few amount of water flowing actually…R0015257.JPG

Going down is the most terrifying part… R0015262.JPG