Friday, February 22, 2013

Jardim Botânico da Universidade de Lisboa

Jardim Botânico da Universidade de Lisboa 2012 março

Rondeletia amoena, Jardim Botânico da Universidade de Lisboa 2012 março

Jardim Botânico da Universidade de Lisboa 2012 março

Senecio petasites, Eucalyptus, Jardim Botânico da Universidade de Lisboa 2012 março

Dracaena draco, Jardim Botânico da Universidade de Lisboa 2012 março 

Click here for more photos of the Jardim Botânico da Universidade de Lisboa. 

The Jardim Botânico da Universidade de Lisboa is a scientific garden that was designed in the mid-19th century to complement botanical teaching and research. Planting was begun in 1873. An enormous diversity of plants were collected by its first gardeners from Portuguese colonies around the world. Most of the garden flows down a hillside with walks, stairs, terraces, ponds & flowing water. It's a bit of a wonderland, a green oasis in the heart of Lisbon, lush & thick with plants, hidden within the busy city near the Avenida Metro Station. The present garden has species from New Zealand, Australia, China, Japan and South America which flourish in the mild Lisbon climate. Many of the plants are quite mature. There are huge Eucalyptus & palm trees, as well as succulents, bromeliads, many Cycads & Mediterranean Fan Palms (Chamaerops humilis) & flowering shrubs I had never seen before.

Friday, February 15, 2013

High Point Natural Drainage System

High Point Natural Drainage System February 2013. Storm water is stored in this large, permanent pond before it empties into Longfellow Creek.

High Point Natural Drainage System February 2013. A cut in the curb allows water from the street to flow into a swale.

High Point Natural Drainage System February 2013. Nearly all the parking strips at High Point have been built as swales.

High Point Natural Drainage System February 2013. A small temporary retention pond.

High Point Natural Drainage System February 2013. A drain at the bottom of a swale.

Because of its size & relationship to Longfellow Creek, the redevelopment of High Point in West Seattle offered Seattle Public Utilities an opportunity to contruct a large natural drainage system, the largest built by the City of Seattle & the first natural drainage system of this scale used in a high-density Seattle neighborhood. Designed in partnership with the Seattle Housing Authority, the system treats about 10 percent of the watershed feeding Longfellow Creek, which flows into the Duwamish River, then Puget Sound. The natural drainage system mimics nature by using swales to capture & naturally filter storm water. Landscaped ponds hold the overflow. All 34 blocks of the High Point community are part of this system. In addition, porous surfaces make up a significant part of the sidewalks & parking spaces. 

High Point was originally developed during World War II to provide government housing. It remained a district of predominantly low-income housing through the 1990s. In 2003, the Seattle Housing Authority began work on the first phase of a 6-year project to redevelop High Point into a mixed-income community. All existing housing, roads & utilities were replaced. High Point now has approximately 1,600 housing units, about half of them low-income rentals owned by the Seattle Housing Authority. The other half are single family homes, condominiums & town homes sold to private owners. 

The need to improve the water quality of Longfellow Creek drove the plan to connect High Point with the surrounding environment. The City of Seattle is required by the US Environmental Protection Agency to dramatically cut sewage overflows by 2025. Natural drainage systems are an effective method for curbing storm water, which can trigger overflows of raw sewage. The swales & temporary retention ponds (also known as rain gardens) are planted with red-twig dogwood, evergreen huckleberry, sword fern, grasses, sedges & other plants. Rainwater soaks into the ground rather than flowing into the (unfortunately combined) storm water & sewer system. Oil, pesticides & other pollutants are filtered out to decompose & be consumed by micro-organisms in the soil.  Not long after a heavy rainfall, swales & shallow ponds are mostly empty of water.  Before flowing on to Longfellow Creek, water is stored in a large pond, often used by migratory waterfowl, located at the lower edge of the development. Following the path of the water through High Point is a pleasant & interesting walk.

Friday, February 8, 2013

January in Seattle

Lincoln Park January 2013

Kerry Park January 2013

Thuja plicata on Queen Anne Hill January 2013

Seattle Center January 2013

Liquidambar styraciflua in Wedgwood January 2013

January 2013 in Seattle was significantly colder & drier than normal.  The mean temperature was 38.2F/3.44C.  The normal mean temperature is 42F/5.55C.  The highest temperature was 53F/11.66C on 1/8, the lowest was 24F/-4.44C on 1/13.  Total precipitation was 4.16 inches.  Normal precipitation is 5.57 inches.  There was 1 day with heavy rain, 2 days with rain, 17 days with light rain, 1 day with light snow, 25 days with fog, 11 days of fog with visibility at less than 1/4 mile, 4 days with haze, 23 cloudy days, 5 partly cloudy days & 3 fair days.      

It was very unusual that no rain fell for 12 days between 1/11 & 1/22.  It was fairly cold, with highs mostly below 40F/4.44C & lows below freezing every night.  But even without rain, it was very moist.  The ground remained wet, with frost every morning & thin ice in places.  6 consecutive days of fog came at the end of this period, sometimes quite heavy & lingering throughout the day.  The weather returned to normal on 1/23 with rain & temperatures well above freezing.  The fog was beautiful, yet oddly inhibiting.  I did not go out walking, or work in the garden.