scholarly journals Review of "El Niño, La Niña, and the global sea level budget" by Piecuch and Quinn

2016 ◽  
Author(s):  
Anonymous
Keyword(s):  
El Niño ◽  
El Nino ◽  
La Niña ◽  
La Nina ◽  
2014 ◽  
Vol 58 (2) ◽  
pp. 302-325 ◽  
Author(s):  
Małgorzata Świerczyńska ◽  
Tomasz Niedzielski ◽  
Wiesław Kosek
Keyword(s):  
El Niño ◽  
El Nino ◽  
La Niña ◽  

2014 ◽  
Vol 4 (1) ◽  
Author(s):  
Habib B. Dieng ◽  
Anny Cazenave ◽  
Benoit Meyssignac ◽  
Olivier Henry ◽  
Karina von Schuckmann ◽  
...  

AbstractInterannual fluctuations of the global mean sea level are highly correlated with El Niño-Southern Oscillation (ENSO) events, with positive/negative anomalies during El Niño/La Niña. In a previous study we showed that during the 1997 - 1998 El Niño, a positive anomaly observed in the global mean sea level was mostly caused by an increase of the ocean mass component rather than by steric (thermal) effects. This result was related to an increase of precipitation over the tropical ocean and a deficit in land water storage. In the present study, we investigate the effect of the recent 2008 and 2011 La Niña events on the satellite altimetry-based global mean sea level. We find that the large global mean sea level drop associated with the 2011 La Niña results from the combined decrease of the steric and ocean mass components, with a slightly dominant contribution from the latter. We show that the ocean mass contribution to the global mean sea level drop is spatially confined over the north eastern tropical Pacific (just as was found previously for the 1997 - 1998 El Niño, but with opposite sign). Corresponding ocean mass spatial pattern is closely correlated to observed sea level and steric spatial patterns over the duration of the La Niña event. This is also observed for previous El Niño and La Niña events. Such a drop in ocean mass during ENSO in the eastern part of the tropical Pacific has not been reported before. It is possibly related to a temporary decrease in the net precipitation over the north eastern Pacific (opposite situation was found during the 1997 - 1998 El Niño).


2020 ◽  
Author(s):  
Fan WANG ◽  
Qiuping Ren ◽  
Yuanlong Li ◽  
Fei Zheng ◽  
Jing Duan

2015 ◽  
Vol 73 (5) ◽  
Author(s):  
Mohd Hilmi Abdullah ◽  
Mohd Razali Mahmud ◽  
Nor Ainah Amat

The El Nino/La Nina Southern Oscillation (ENSO) phenomenon indirectly provides dramatic changes to tidal that can cause floods, drought and affect various marine activities. Tidal observation data plays important role in determining the characteristic or behaviour of tide along the coastal area especially during sudden climate change such as the phenomenon of El Nino/La Nina, the Northeast Monsoon, Northwest Monsoon and Tsunami. It is important to study the occurrence of the ENSO event and it characteristic so that it can be used for prediction and monitoring the land and water ecosystem. This research is to identify the variations of sea level and tidal behaviour in Malaysian coastline during El Nino/La Nina. The tidal observation data, meteorology data (temperature and mean sea level pressure), and Southern Oscillation Index (SOI) calculation are used to look on the changes of the tidal variation during the ENSO phenomenon. The results of this research will specially benefit in the determination of tidal level in Malaysia and to the professionals who have responsibilities in policy making, agriculture, environmental planning, economics and marine engineering.


2019 ◽  
Vol 38 (1) ◽  
pp. 55
Author(s):  
Yusdar Hilman ◽  
Suciantini Suciantini ◽  
Rini Rosliani

<p>Horticultural products (fruits, vegetables and ornamental crops) which have high competitiveness and added value, require supporting appropriate cultivation technology. The objective of this paper was to sort out adaptive technologies that can be implemented for horticultural cultivation, especially on dry land, to minimize yield loss due to climate changes. Horticultural crops in dry lands faced various problems. Characteristics of horticultural crops, among others were easily damage, bulky, sensitive to water stress and the incidence of pests and diseases. Another issue that has begun to happen in the field is the occurrence of extreme climate change, especially El Nino or La Nina that caused crop failures, damage to agricultural land resources, increased in frequency, extent, and intensity of drought, increased moisture, increased in the susceptibility to pests and the disease. Thus the integrated efforts that are needed in strengthening the capability of dry land to face climate change are by the application of adaptative technology, drafting disaster mitigation concepts, observing climate change, policy analysis related to the application of adaptive technology on climate change. The discussed Horticulture Commodities are focused on economically profitable crops, including: vegetables (potatoes, shallots, chili), fruits (bananas, citrus and melons) and ornamental crops (chrysanthemums, orchids, Polycias and Gerbera) scattered in two zoning zones where namely (i) lowland (0-600 meters above sea level); (ii) highlands (&gt; 600 meters above sea level) and (iii) in both elevations of the site which have wet climates and dry climates. Attempsto be made to promote horticultural crops include performing water-efficient irrigation (drip irrigation), mulching, the use of shading on certain crops, proper fertilization, the use of organic fertilizer, planting system and planting distance, and tolerant varieties. Some adaptative technologies that can be adopted for horticultural crops include (1) developing watersaving irrigation technologies (drip and sprinkler irrigation on shallots), (2) applying healthy crop cultivation (good quality seeds, variety tolerant to disease and sub-optimal environment for tomatoes, red or hot chilli shallots and bananas), (3) using environmentally friendly chemical control (concept of threshold control in red or hot chilli), (4) protecting yield and quality of harvest (the use of silver black mulch on shallots and melons, and the use of shade for ornamental plants on dry land).</p><p>Keywords: Horticulture, climate change, upland, adaptation technology</p><p> </p><p><strong>Abstrak</strong></p><p>Sistem produksi hortikultura (buah buahan, sayuran, dan tanaman hias) yang berdaya saing tinggi dan bernilai tambah memerlukan dukungan teknologi. Tulisan ini merangkum teknologi adaptasi komoditas hortikultura pada lahan kering dalam upaya meminimalisasi tingkat kehilangan hasil akibat perubahan iklim. Usaha tani tanaman hortikultura pada lahan kering dihadapkan pada berbagai masalah, di antaranya tanaman mudah dan cepat rusak, sensitif terhadap cekaman lingkungan, dan rentan terhadap hama dan penyakit. Masalah lain yang berdampak negatif terhadap sistem produksi komoditas hortikultura ialah perubahan iklim ekstrem, terutama el-nino dan la-nina. Perubahan iklim tidak hanya menyebabkan kegagalan panen, tetapi juga merusak sumber daya lahan pertanian, meningkatkan luas areal dan intensitas tanaman yang mengalami kekeringan, meningkatkan kelembaban, dan perkembangan hama dan penyakit tanaman. Oleh karena itu diperlukan integrasi pengelolaan lahan dan aplikasi teknologi adaptif perubahan iklim, penyusunan konsep mitigasi bencana, observasi perubahan iklim, dan analisis kebijakan yang terkait dengan aplikasi teknologi adaptasi terhadap perubahan iklim. Pembahasan difokuskan pada tanaman yang secara ekonomi menguntungkan, antara lain kentang, bawang merah, cabai untuk komoditas sayuran; pisang, jeruk, dan melon untuk komoditas buah-buahan; dan krisan, anggrek, polycias dan gerbera untuk tanaman hias. Komoditas hortikultura tersebut tersebar di dua zonasi ketinggian tempat, yakni dataran rendah (0–600 m dpl) dan dataran tinggi (&gt; 600 m dpl). Beberapa teknologi adaptasi yang dapat diadopsi di antaranya (1) irigasi hemat air (irigasi tetes dan irigasi curah pada bawang merah), (2) budi daya tanaman sehat (benih bermutu, varietas toleran penyakit dan lingkungan suboptimal untuk komoditas kentang, cabai, bawang merah, dan pisang, (3) pengendalian hama dan penyakit ramah lingkungan (konsep ambang pengendalian pada cabai, jeruk), dan (4) perlindungan hasil dan peningkatan kualitas hasil panen (penggunaan mulsa plastik hitam perak pada tanaman bawang merah dan melon, serta penggunaan naungan pada tanaman hias anggrek dan krisan). Kata kunci: hortikultura, perubahan iklim, lahan kering, teknologi adaptasi</p>


MAUSAM ◽  
2021 ◽  
Vol 52 (1) ◽  
pp. 57-66
Author(s):  
G. C. ASNANI

El-Nino of 1997-1998 was accompanied by severe global weather anomalies, which generated widespread interest at all levels in the world. As a result, United Nations General Assembly passed a resolution (52 / 200) urging International co-operation to reduce the adverse impact of El-Nino on human society and Environment. The El-Nino (Warm Phase) commenced around April – May 1997, reached peak intensity around December 1997 and ended around May 1998. La-Nina (Cold Phase) started around this time, reached its peak in January 1999, weakened around June - July 1999 and has continued in its weak phase at the time of writing, August 1999.   Development and decay of the El-Nino are illustrated through SST,SOI and sea-water temperature below the sea-surface. Features during peak period of El-Nino are illustrated through SST, sea-level pressure, surface wind, OLR, and Walker Circulation. There is clear evidence of west-to-east propagation of OLR anomaly, 850 hPa zonal wind anomaly and sea-level pressure anomaly. SST anomaly pattern did not give strong evidence of this type of zonal progression.   El-Nino is global in nature.   El-Nino / La-Nina years during the 120-year period 1871-1990 are tabulated along with All India Summer Monsoon Rainfall (AISMR) anomalies. There is evidence of El-Nino years tending to become years of deficit rainfall and La-Nina years being years of excess rainfall over India. El-Nino / La-Nina events, which can be predicted 6-12 months in advance, can be used and are being used as part of the prediction formulae, in the issue of official monsoon rainfall forecast by India Meteorological Department. Based on El-Nino considerations alone, it has been feared, in some quarters, that 1997 might become a year of extreme deficit summer monsoon rainfall. However, the actual rainfall over India during June – September 1997 was 2 % above normal. India Meteorological Department had predicted "normal" rainfall (+-10% of the rainfall).


Author(s):  
Riyadi . ◽  
Adri A Tarumingkeng ◽  
Rignolda Djamaluddin ◽  
Gybert E Mamuaya

Coastal Waters of Lembeh Strait characterizes by small waves and bathymetry undulation. While Sangihe waters have big waves, coastal bays with gently sloping beaches and flawless beaches that are generally steep headlands or cliffs on the shoreline. Differences in these two characters are interesting to watch, especially the value of the Mean Sea Level (MSL). The Least square method is the method of calculating the tidal harmonic constants which are the amplitude and phase lag. Formzahl number calculation is used to determine the type of the tidal in these two waters. The Formzahl numbers of these two waters ranged from 0.26-1.5, so there was no difference in the tidal type. The type of tidal of these two waters was catagorised as Mixed Tide Prevailing Semidiurnal, which is generally in eastern Indonesia waters. Comparison of the fluctuation of Mean Sea Level (MSL) in Lembeh Strait waters in normal climatic conditions, lanina and elnino showed the difference in height. In elnino condition, the MSL value was 87 mm lower (5.9%) than in normal operating condition (1387 mm), and in lanina condition, the average of MSL was higher 51 mm (3.46%) of the normal condition (1525 mm). While in normal climatic conditions, the MSL was 1474 mm© Perairan laut di Selat Lembeh mempunyai karakteristik gelombang kecil dan batimetri berundulasi.  Sedangkan di perairan Sangihe memiliki gelombang besar, pantai teluk berparas pantai landai dan pantai tanjung yang umumnya terjal atau bertebing pada garis pantai. Perbedaan dua karakter ini menjadi hal yang menarik untuk diamati, terutama muka air laut rerata (MLR). Metode least square adalah metode perhitungan pasang surut yang digunakan untuk menghitung konstanta harmonik yaitu amplitude dan kelambatan fase. Dengan perhitungan bilangan Formzahl akan mengetahui tipe pasang surut di kedua perairan tersebut. Diperoleh bilangan Formzahl perairan tersebut berkisar antara 0,26-1,5, sehingga tidak ada perbedaan tipe pasang surutnya. Tipe pasang surut antara kedua perairan ini adalah tipe pasang surut campuran condong ke harian ganda. Pasang surut jenis ini banyak terdapat di perairan Indonesia bagian timur.  Perbandingan fluktuasi muka laut rerata (MLR) di perairan Selat Lembeh pada kondisi iklim normal, El Niño dan La Niña menunjukkan perbedaan ketinggian. Di mana pada kondisi El Niño mempunyai muka laut rerata (MLR) lebih rendah 87 mm (5,9%) dari kondisi normalnya yaitu 1387 mm dan pada kondisi La Niña mempunyai muka laut rerata (MLR) lebih tinggi 51 mm (3,46%) dari kondisi normalnya yaitu 1525 mm. Sedangkan pada kondisi iklim normal muka laut rerata (MLR) adalah 1474 mm©


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