Wednesday, January 16, 2008

Fossils of a 300-Million-Year-Old Forest Found (01.15.2008 )

Fossils of a 300-Million-Year-Old Forest Found

by Michael Abrams (Discover Magazine)

“The woods are lovely, dark and deep,” Robert Frost wrote when moved by the sight of a contemporary forest. But a coal mine in Illinois has revealed woods that, if not lovelier, are certainly darker and deeper—and a good bit older.

“You can walk in a single direction for a long distance, through this bizarre Lord of the Rings, cathedral-like thing,” says Scott Elrick, a geologist with the Illinois State Geological Survey, who studied the 300-million-year-old fossilized forest. “As you look up, you see gray flat shale, impressions on that shale, or entire trees, or tree stumps. . . . It’s the worm’s-eye view. You’re looking up at what the forest floor used to look like.”

The fossil ceiling, held up by 6-foot-high, 80-foot-wide pillars of coal, goes on for 4 square miles. No other known preserved forest comes close in size. And thanks to tidal rhythms, the mud deposited on top of this forest is layered, so years can be counted as with the rings of a tree. The 15 feet of sediment that blankets the fossils was laid down in four months—instantaneously in geologic time. The mine runs along a fault line, leading Elrick to surmise that an earthquake dropped one side of the fault and caused flooding. Because the subsequent influx of sediment was “not a catastrophic tsunami thing but more of a slow-motion event, all the small itty-bitty plants are in place.”

The slow pace at which that mud flowed in preserved an incredible diversity of flora. “We had lycopod trees 6 feet wide and 100 feet long, ground cover things, sphagnum moss, delicate little ferns next to these big, huge, honking trees. It’s crazy—we haven’t seen anything like this before,” Elrick says. At the moment, no one else is likely to see it either: The mine, now empty of coal, is closed.

Tuesday, January 08, 2008

Paradoks Wildavsky? - Rabu, 09 Januari 2008 (Opini Kompas)

Paradoks Wildavsky?

Jonatan Lassa

"Any failure to mitigate hazards is shown up in their impacts." (Prof David Alexander)

Jika perlu diringkaskan dalam dua kata tentang kemajuan pengelolaan bencana di Indonesia dalam tiga tahun kepemimpinan SBY-Kalla, penulis menyebutnya sebagai Paradoks Wildavsky, yang diartikan sebagai paradoks doing better, feeling worst.

Di atas kertas, SBY-Kalla patut berbangga karena kebijakan penanganan bencana mereka lebih baik dari rezim-rezim sebelumnya. Mulai dari UU Bencana No 24/2008, Rencana Aksi Nasional Pengurangan Risiko Bencana, hingga masuknya anggaran mitigasi bencana dalam APBN.

Berpikir jangka panjang?

Mencermati kejadian banjir Bengawan Solo, penulis belum melihat horizon pemikiran jangka panjang saat Wapres Jusuf Kalla menegaskan "akan melakukan langkah fundamental, menyeluruh, dan bersifat jangka panjang dalam penanggulangan bencana alam banjir dengan pelaksanaan gerakan penanaman satu juta hektar lahan (Gerhan)" (Kompas, 4/1/2008).

Yang pasti, bencana tidak (tetapi kadang) seperti "cinta" yang subyektif, tergantung siapa yang memandang. Bila yang memandang banjir adalah LSM dan pemerhati lingkungan, alasannya klasik, hutan gundul dan pembalakan liar. Ini sering dikenal dengan one-size-fits-all approach. Pendekatan ini terlihat jelas dalam jurus standar Gerhan itu.

Jika ahli teknik yang melihat, sangat mudah ditebak alasan yang dikemukakan, yakni pendekatan teknis engineering yang dipakai. Pengetahuan inilah yang dominan mendorong lahirnya kebijakan khas teknokrat yang tercermin dalam gagasan Menteri Pekerjaan Umum, yang "berjanji akan membangun 20 waduk pengendali banjir" di DAS Bengawan Solo (Kompas, 4/1/2008) dengan justifikasi teknis yang tidak bisa serta-merta disalahkan.

Pada dasarnya, kedua pendekatan itu tidak salah dan saling melengkapi. Namun, ini tidak cukup karena secara empiris, gabungan skenario waduk dan Gerhan tidak serta-merta menyelesaikan banjir, karena itu tidak cukup disebut "pendekatan jangka panjang".

Horizon yang panjang baik dari sisi sejarah bencana (kronologis, rekaman perilaku dalam lintasan zaman, cerita rakyat, hikayat banjir, memori kolektif, dan rekaman Jawa kuno) seharusnya menjadi soko guru agar kita tidak panik dan menafikan pengetahuan lokal yang dinamis dalam penanganan banjir di Solo.

Studi sosiologi bencana juga sering absen dalam analisis banjir di Indonesia. Alhasil, banjir masih dilihat sebagai external agents—yang asing, yang dari alam, dan direduksikan sebagai bencana alam—mirip konsep penanganan bencana di Amerika Serikat 50 tahun lalu, tepatnya pasca-Perang Dunia II, saat lembaga-lembaga penanganan bencana adalah bekas lembaga perang saat itu yang memandang banjir dan tornado mirip bom yang hendak dijatuhkan musuh dari atas, yang sulit dikontrol.

Dalam studi bencana, hal ini dinamakan hantu "paradigma perang" yang menghantui praktik penanganan bencana baik di berbagai tempat, termasuk di Indonesia. Sindrom pasca-Perang Dunia II itu masih ditelusuri dalam UU Bencana No 24/2008, terlihat dalam kata "bencana alam", yang juga diulangi oleh Wapres dengan "bencana alam banjir" (Kompas, 4/1/2008).

Belajar dari Belanda lagi?

Dalam konteks pengetahuan penanganan banjir di Indonesia, sebagian bahkan merupakan reproduksi ulang dari zaman Belanda dengan data sejarah banjir sejak abad ke-17 dengan visi pemerintah kolonial dalam menjadikan Jakarta (Batavia) sebagai Amsterdam Baru, yang berfungsi sebagai waterfront city (Caljow et al 2004).

Patut diakui, Belanda adalah negeri yang secara gemilang menghentikan banjir sebagai kutukan alam dengan sejarah yang relatif panjang. Di Belanda, politisi mampu melihat jarak yang panjang antara kejadian banjir dan peristiwa bencana. Entah mengapa, di Indonesia, politisi kerap melakukan short-cut, banjir sama dengan bencana?

Hingga awal abad ke-14, sebagian wilayah darat Belanda masih merupakan daerah genangan. Hal ini menyulitkan penduduk setempat mengklaim kepemilikan lahan. Bisa dimaklumi, jika permukaan laut lebih tinggi, air pasang akan selalu mengaburkan konsep kepemilikan lahan, dan ini diperburuk oleh banjir yang berkajang (Oft and Tsuma 2006).

Periode abad ke-15-16 ditandai giatnya pembentukan polder penahan pasang. Hal ini ditopang kelembagaan lokal yang dibentuk secara demokratis dengan kecirian mobilisasi diri. Dewan keairan (waterschappen) juga mulai terbentuk. Era ini juga ditandai dibentuknya Rijkwaterstaat, semacam "Lembaga Nasional Pengelola Pantai dan Keairan".

Waterschappen kemudian diformalkan tahun 1815 dalam mandat, dengan menangani banjir berkoordinasi erat dengan Rijkwaterstaat. Kerja sama ini masih efektif hingga akhir abad ke-20.

Rantai perkembangan pengetahuan penanganan banjir di Belanda bisa ditelusuri karena dokumentasi pengetahuan yang baik. Tidak terjadi apa yang disebut sebagai hilangnya mata rantai pengetahuan (knowledge loss) tentang banjir di konteks lokal.

Kontras dengan perbedaan persepsi antara Bupati Tuban yang mengatakan, pusat tidak menyetujui usulan tanggul banjir yang diusulkan tiap tahun (Kompas, 5/1/2008). Sedangkan Menko Kesra mengklaim, pusat sudah peduli mitigasi bencana kecuali bahwa daerah tidak memberi perhatian dan ditambahkan "daerah kurang sarana pendukung seperti pesawat helikopter yang bisa dipakai untuk memantau dan memasok bantuan serta obat-obatan" (Kompas Cyber Media, 3/1/2008).

Diktum Prof David Alexander itu bisa disimpulkan sementara bahwa skala dramatis bencana hari ini adalah penegasan atas kegagalan ekonomi politik, termasuk gagal dalam cara pandang menangani bencana dalam perspektif jangka panjang.

Jika di awal tulisan ini asumsinya adalah paradoks Wildavsky, di akhir tulisan ini bisa disimpulkan sebaliknya dalam menjelaskan kemajuan tata kelola bencana Indonesia, yakni feeling better, doing worst.

Jonatan Lassa - PhD Researcher in Disaster Governance, ZEF, University of Bonn

Friday, January 04, 2008

Status Quo Of The Tsunami Early Warning System For The Indian Ocean

The German-Indonesian Tsunami Early Warning System for the Indian Ocean (GITEWS) runs on track। Main milestones like the development of the automatic data processing software SeisComP3, as well as the underwater communication for the transmission of the pressure data from the ocean floor to a warning centre are already finalised. Furthermore the calculations of the ocean modelling including the source modelling were completed and are available in a data base so that the system can be set into operation at the end of 2008. This positive conclusion is drawn by the GITEWS consortium consisting of different German geo and marine scientists on the occasion of the third anniversary of the tsunami catastrophe on December 26, 2004.

After the severe earthquake, where almost a quarter of a million people lost their lives, the German government requested the Helmholtz Association of National Research Centres, represented by the GeoForschungsZentrum Potsdam (GFZ, Germany's National Lab for Geosciences) to develop a tsunami early warning system. Already three weeks after the natural disaster a task group headed by the GFZ submitted a concept for GITEWS to the German government. This concept is based on different kinds of sensor systems on land and on the ocean and goes along with an intensive education and training programme. "The GFZ is working in Southeast Asia since 1992 so these broad geoscientific results could flow into the proposal in a quick reaction" explains Professor Reinhard Hüttl, chair of the executive board of the GFZ. "We would also like to establish this warning system in other endangered regions, such as in the Mediterranean and in the Atlantic."

The tsunami early warning system is financed with 45 Mio. Euros by the Federal German Ministry for Science and Education and come from the 500 Mio. Euro budget of the German Federal Government for reconstruction activities in the tsunami region.

Seismological components
In 90% a tsunami is caused by a submarine earthquake. The quake in December 2004 had magnitude of 9.3, the second largest ever detected rupture in the earth crust. A fast and correct seismological recording and evaluation is therefore essential for the warning system. The biggest challenge is the failure-free recording and the exact quantification of strong quakes close to the epicentre. With the seismic sensors installed so far in Indonesia and with the GFZ developed software system SeisComP3 which was launched in May 2007, there is now for the first time a tool to quickly register and evaluate even strong earthquakes.

Its capacity and functionality has been demonstrated several times: the magnitude of 8.0 and the location of the Bengkulu quake in the southern part of Sumatra on September 12, 2007 could be determined within four minutes. Based on that information the Geophysical Survey in Jakarta (BMG) released a tsunami warning based on these data for the first time.

Meanwhile SeisComP3 is established as standard in several states bordering the Indian Ocean such as in the Indian tsunami warning centre. The tsunami warning centre for the Mediterranean and the North Atlantic will also go into service in 2008 with this software. "With the software technical and methodical development within GITEWS we set new standards not only specifically for earthquake monitoring but also for the tsunami warning" said Dr. Winfried Hanka, project leader for the GITEWS earthquake monitoring at the GFZ.

Oceanographic components
Based only on seismological measurements it is impossible to decide whether a tsunami has arisen or not. Therefore the detection of a tsunami is carried out directly on the ocean floor using oceanographic instruments. These measurements are also important to give the all-clear, because not every earthquake generates a tsunami. This additional information is very important for Indonesia, because earthquakes are easily sensible at the coast and could give rise to panic reactions. So a warning and an all-clear warning respectively need to be given very fast. To meet these expectations different components are established in the GITEWS concept.

Buoy systems

The final system will consist of 10 buoys, which will be deployed along the Sunda arch off the Indonesian coast. The buoys have two functions: they work as a relay station for the data of the underwater pressure sensors (OBU - ocean bottom unit) transmitting their data from the sea floor to a modem close to the water surface and from there via the satellite connection of the buoy to a warning centre. Furthermore the buoy has different sensors to determine meteo data and the sea swell. But the pioneering aspect of the buoys is the GPS functionality: through GPS measurements it is also possible to detect a tsunami independent of the measuring instruments on the ocean floor.

This is an important progress compared to other buoy systems used for example in the Pacific Ocean। The combination of underwater and surface measurements guarantees a higher availability and less breakdowns. Dr Tilo Schöne, GFZ Potsdam, leader of the GPS buoy working group as well as of the tide gauges working group announced: "Based on the experiences made with two test systems in Indonesia eight more systems will be prepared and deployed in summer 2008 along the coastline of Sumatra and Java. These buoys will be important components for the early warning system."
Ocean bottom units (OBUs)

To recognise water pressure changes caused by tsunami waves, ocean bottom units are installed on the ocean floor. In addition to this standard measuring method GITEWS uses specific seismometers to detect an earthquake directly on the sea floor. The challenge is not only the measurement but also the transmission of the data through the 4 km large water column. The first tests with commercial modems did not fulfill the technical requirements because transmitting the signal in thermally and salinary layered ocean water through more than four kilometres is not trivial. In co-operation with small and midsize enterprises it was possible to develop a new transmission technology.

"The so-called PACT bottom pressure system (Pressure based acoustically coupled Tsunami detector) is used for the real-time detection of sea level changes in the deep ocean. In November 2007, the PACT system successfully passed a deep-sea test close to the Canaries" emphasises Dr. Olaf Boebel, PACT project leader from the Alfred-Wegener Institute for Marine and Polar Sciences.
Tide gauge measurements

In deep water a tsunami propagates with the same speed as an aircraft. But in shallow water the tsunami wave looses its speed and gains height - up to 30 meters - close to the coastline. Therefore, it is important to register a tsunami in suitable regions e.g. offshore islands. Meanwhile seven GITEWS tide gauges have been installed in the Indian Ocean, not only in Indonesia, but also in riparian states. Reliable tide gauges data are available from South Africa (Marian Island), Yemen (Aden) and Iran (Chabahar). "Tide gauges measurements allow for a reliable prognosis if a tsunami wave is expected and in which dimension. So it is possible to receive detailed information of the inundation, which is especially of importance for densely populated areas such as Padang" explains Tilo Schöne Simulations.

Tsunami-simulations are of particular importance for the whole warning process. Based on a few measured data an overall picture has to be calculated. A couple of minutes after the earthquake the modelling results will give an estimation on the wave height, the time of arrival and the inundation areas. Combined with the information on the settlement structure in affected coastal stretches this is valuable information for the authorities and the population. Since warning times in Indonesia are extremely short, thousands of different scenarios are pre-calculated. According to measured event data the best-fit scenarios are selected from this data base which compriseall the necessary data like arrival time, wave height and risk evaluation. This assessment of the situation will be continuously improved taking more and more measured data into consideration.

The data gained from this simulation also provides the basis for the alarm of remote areas threatended by the tsunami such as India, Sri Lanka or East Africa. "The concurrent utilisation and analysis of all available data allows - for the first time - a precise prediction of the inundation in the influenced regions in an extremely short time scale. TsunAWI, the new tsunami simulation software based upon calculations on unstructured triangle grids which was developed at AWI and the innovated GFZ modelling of the earth crust deformation/movement, are the basis for this new achievement" underlines Dr. Jörn Behrens coordinator of the GITEWS simulation group.
The Warning Centre

The core of the early warning system is the warning centre. All sensor data converge here, from here all the instruments are controlled, and here the synthesis of all data and the pre-calculated simulations is done and the alarm is given. These different activities are integrated in a decision support centre (DSS), which provides the responsible officer with an overview of the available data, an assessment of the situation and proposals for decision.This system, seen from the viewpoint of conceptual design and complexity, is unique worldwide. The development of the DSS is done by the German Aerospace Centre (DLR) and is in good progress. At the beginning of 2008 the first prototype will be installed in Indonesia.

Civil defence, Education and Training programme
The fastest warning is useless as long as the gap to the so called "last mile to the beach" is not closed. The population in the threatened area needs to be informed in time, but they also need to be trained how to react properly. The people need to be informed about evacuation plans and how to behave in the case of emergency. Japan carries out this kind of training in schools, plants and companies on a regular basis. The establishment of such an education programme in the areas bordering the Indian Ocean has only just started.

In addition, there is an academic education and training programme with regular training courses for different sensor groups or risk modelling for experts and scientists.

Furthermore the "Gesellschaft für Technische Zusammenarbeit" (GTZ) in three pilot regions enhances civil defence activities which aim in particular to the development of necessary institutional and organisational capacities. Members of the German Federal Agency for Gesciences and Ressources (BGR) continue with this consulting on the national level.

Also, a PhD and post doc programme is carried out by the United Nations University (UNU) to guarantee the operation and future upgradingof the GITEWS from the scientific point of view. "Offering this variety of education possibilities makes an important contribution to the early warning system for Indonesia and other bordering states of the Indian Ocean", says Prof. Torsten Schlurmann, Director of the Franzius Institute for Hydraulic and Civil Engineering at the Leibniz University in Hannover. Prof. Schlurmann leads the Capacity Building programme on behalf of the UNU together with colleagues from the GTZ.

A Look into the Future

"The technical system of GITEWS will be established till the end of 2008, on the condition that no unpredictable events occur such as the natural disaster in December 2004 . At the beginning of 2009 we will operate the system together with our Indonesian colleagues. In 2010 the system will be handed over completely to the Indonesian partners", explains the project co-ordinator Dr. Jörn Lauterjung of the GFZ.

Vulnerability analyses, carried out in Indonesia within the GITEWS project, indicate that it is essential but also possible to be prepared. However, complete protection will ever be impossible, even with a technically perfect warning system. Natural hazards such as earthquakes clearly demonstrate the elemental forces of our planet . "Our aim is to minimize the number of victims", says Dr. Lauterjung and explains: "Even more than eight hours after the severe earthquake in 2004 and more than 6000 of kilometres away from the epicentre, over 300 of people were killed. Natural catastrophes of such a size will always claim many lifes. But this huge number of victims could have been reduced very much with an Early Warning System."

This aterials provided by http://marineanimalnews.blogspot.com with reference to Helmholtz Association of German Research Centres.