JOhnson Outdoors Inc.,约翰逊户外产品公司(美国)http://www.jwa.com/Email:corporate@johnsonoutdoors.com是美国一家主要研制生产销售户外产品的企业,主要产品包括钓具、潜水装备、救生衣、帐篷等等。从网上可查询到公司简介、地理...JOhnson Outdoors Inc.,约翰逊户外产品公司(美国)http://www.jwa.com/Email:corporate@johnsonoutdoors.com是美国一家主要研制生产销售户外产品的企业,主要产品包括钓具、潜水装备、救生衣、帐篷等等。从网上可查询到公司简介、地理位置、投资关系、就业机会、产品类别以及设在世界各地的分公司的情况等方面的信息。展开更多
Antisana is a stratovolcano with an associated glacier located in the Ecuadorian Andes. Dr Aguirre made meteorological readings every day, at every hour from sunrise to sunset, from December 1845 to December 1846, at ...Antisana is a stratovolcano with an associated glacier located in the Ecuadorian Andes. Dr Aguirre made meteorological readings every day, at every hour from sunrise to sunset, from December 1845 to December 1846, at Antisana using a meteorological station at 4060 mamsl （meters above mean sea level）. Unfortunately, only the monthly average data have been preserved. These meteorological data are here studied and compared with the closest modern stations for monthly values of temperature, rainfall, and pressure. According to these comparisons, the year 1846 was rainy and cold in comparison with the current climate. Moreover, these observations have been useful to help resolve a debate about a possible E1Nifio event in 1846 with the high precipitation in Antisana and Quito in 1846 discarding the occurrence of an E1 Nifio event. The probable occurrence of a La Nifia event is discussed. These data are the earliest known systematic instrumental meteorological observations taken at above 4000 mamsl.展开更多
基金supported by the PROMETEO project,Secretariat of Higher Learning,Science,Technology and Innovation(Ecuador Government)the project PIS-1403EPNpartially financed by FEDER-Junta de Extremadura(Research Group Grant GR15137)
文摘Antisana is a stratovolcano with an associated glacier located in the Ecuadorian Andes. Dr Aguirre made meteorological readings every day, at every hour from sunrise to sunset, from December 1845 to December 1846, at Antisana using a meteorological station at 4060 mamsl （meters above mean sea level）. Unfortunately, only the monthly average data have been preserved. These meteorological data are here studied and compared with the closest modern stations for monthly values of temperature, rainfall, and pressure. According to these comparisons, the year 1846 was rainy and cold in comparison with the current climate. Moreover, these observations have been useful to help resolve a debate about a possible E1Nifio event in 1846 with the high precipitation in Antisana and Quito in 1846 discarding the occurrence of an E1 Nifio event. The probable occurrence of a La Nifia event is discussed. These data are the earliest known systematic instrumental meteorological observations taken at above 4000 mamsl.
